Bibliografi Jawa

BIBLIOGRAPHY OF THE GEOLOGY OF INDONESIAAND SURROUNDING AREAS Edition 6.0, September 2016 J.T. VAN GORSEL III. JAVA, MADURA, JAVA SEA www.vangorselslist.com III. JAVA, MADURA, JAVA SEA This chapter of the bibliography contains 226 pages with 2059 titles on the geology of Java, Madura and the Java Sea. It is subdivided into four areas/ topics: III.1. Java - General, onshore geology III.2. Java Sea (incl. Sunda Basin, offshore NW Java basin) III.3. Java - Quaternary Volcanism III.4. Madura- Madura Straits. The island of Java has a long history of geological studies, dating back to the mid-1800's. Junghuhn (1854) in his famous book on the natural history of Java dispelled the then current notion that all of Java was composed of volcanic rocks. The first monograph dedicated to the geology of Java by Verbeek and Fennema (1896; with the first geologic map) is still the only one. A modern synthesis is badly needed. A new book by Peter Lunt (in press) on the sedimentary geology of Java will fill much of this need. Focus areas of Java geology research have been on structure, volcanism, Eocene- Recent stratigraphy, paleontology, and hydrocarbons, Pleistocene hominids and mammal fossils, etc. S-N cross-section across Central Java (Verbeek and Fennema 1896; part) S-N cross-section across West Java (Gerth 1931). The western part of the Java Sea is a continuation of the Paleozoic- Early Mesozoic continental basement complexes of Sumatra and Borneo. Most of Java island appears to be underlain by Late Cretaceous- Eocene age accretionary complexes and Paleogene arc volcanics. Outcrops of the oldest 'basement' are found in only three relatively small areas in Central (Luk Ulo, Bayah) and SW Java (Ciletuh). It has been suggested from the composition of Quaternary volcanic rocks that parts of East Java may be underlain by oceanic crust. Other evidence, like the presence of Archean-age zircons in E Miocene volcanics of SE Java would suggest the subsurface presence of Australian continental material there (or sediments derived from it). The backbone of Java is a series of relatively young active volcanoes, most of them about 3000m high, and spaced about 80 km apart. A long belt of outcrops of latest Oligocene- earliest Miocene 'Old Andesite' volcanic arc deposits follows today's South Coast (Southern Mountains). These probably formed the only land areas through most of Late Eocene- Pliocene time, when most of the northern half of Java was a marine basin. The present-day land area formed mainly since the Pleistocene by a combination of renewed arc volcanism, an Bibliography of Indonesia Geology, Ed. 6.0 1 www.vangorselslist.com Sept 2016 episode of N-vergent compressional tectonics N of the modern arc and rapid shoreline progradation driven by erosional products of this activity. Oil and gas seeps had been known for a long time in East and Central Java. Descriptions of these started to appear in the literature by the 1850's (Junghuhn 1854, Von Baumhauer 1869). The first shallow oil exploration well was drilled in 1871, at an oil seep near Cirebon in C Java. The first discovery was the Kuti Field in in 1888, near Surabaya, NE Java. This was followed by many other discoveries in the Cepu area at Kawengan (1892) and Ledok (1893). Exploration activity and oil production already started to decline in the 1920's. The traditional plays in NE Java were in M Miocene- Pliocene sands and Globigerina calcarenites in young surface anticlines. Only since the late 1980's has the oil industry become aware of the successful deeper play in Oligocene- E Miocene reefal builups, extending from the Cepu area into Madura Straits. NW Java has been area of oil and gas discoveries since the late 1960's, mainly in the offshore. Like on Sumatra, all oil and gas fields appear to be above, or within migration distance of, two Oligocene rift basins with lacustrine and coaly source rocks, the Arjuna and Sunda basins. Main reservoirs are Late Oligocene- E Miocene Talang Akar/ Cibulakan fluvial- deltaic sandstones and Early Miocene Baturaja limestones. The southern part of the Arjuna basin continues into the onshore, but rapidly deepens towards a young thrust belt and contains mainly small gas discoveries. The Java Sea off East Java- Madura has some some small oil and gas discoveries, but, despite the widespread distribution of Oligo-Miocene carbonate and clastic reservoir rocks, exploration in this area has been rather disappointing. The Java forearc zone has not been successful for hydrocarbons. Surface seeps are not known (except in the Banyumas area of Central Java) and the limited number of wells drilled there were dry. Traditional wisdom blames this on the absence of Eo-Oligocene rift systems and unusually low geothermal gradients. The volcanic belt of West Java has yielded a number of moderate-size gold-silver deposits. Java lacks the commercial Tertiary coal deposits known from S Sumatra and SE Kalimantan. Only a few small-scale coal exploitations are known from the Eocene of Bayat, SW Java and the Middle Miocene Ngrayong Fm at the W end of the Rembang zone, NE Java (figure below) WSW-NE cross-section across M Miocene coal-bearing clastics of W Rembang zone NE Java ('T Hoen 1918). Java has also been a focus area of numerous studies on volcanoes and on Pleistocene mammals and hominids. See more on this under the chapters on these topics. A major milestone publication on the the geology and stratigraphy of Java is the recent book by P. Lunt (2013)- The sedimentary geology of Java (IPA Special Publication, 340 p.) Bibliography of Indonesia Geology, Ed. 6.0 2 www.vangorselslist.com Sept 2016 Suggested reading General, Historic: Junghuhn (1854), Martin (1891), Verbeek and Fennema (1896), Van Bemmelen (1949) Tectonics: Van Bemmelen (1949), Sujanto and Sumantri (1977), Chotin et al. (1980, 1984), Dardji et al. (1994), Soenandar (1997), Sribudiyani et al. (2003), Satyana et al. (2004), Satyana (2005, 2006, 2007), Clements and Hall (2007, 2008), Hall et al. (2007), Clements et al. (2009), Seubert and Sulistianingsih (2008), Granath et al. (2010, 2011) Cenozoic Stratigraphy: Paltrinieri et al. (1976), Suyanto and Sumantri (1977), Baumann (1982), Lunt (2013) Pre-Tertiary: Bothe (1929), Harloff (1929), Tjia (1966), Ketner et al. (1976), Suparka and Soeria-Atmadja (1991), Wakita et al. (1991, 1994), Harsolumakso and Noeradi (1996), Miyazaki et al. (1998), Parkinson et al. (1998), Prasetyadi et al. (2002-2006), Kadarusman et al. (2007, 2010) Volcanism: Bellon et al. (1989), Leterrier et al. (1990), Soeria-Atmadja et al. (1988, 2004), Soeria-Atmadja and Noeradi (2005), Smyth et al. (2006, 2007, 2008) Hydrocarbons NW Java: Arpandi and Sujitno (1975), Burbury (1977), Soulisa and Sujanto (1979), Molina (1985), Wight et al (1986, 1997), Ponto et al. (1989), Yaman et al. (1991), Aldrich et al. (1995), Gresko et al. (1995), Wight (1995), Noble et al. (1997), Nugrahanto. and Noble (1997) Hydrocarbons NE Java: Weeda (1958), Soetantri et al (1973), Soeparyono and. Lennox (1989), Ardhana et al. (1993), Schiller et al. (1994), Willumsen and Schiller (1994), Cole and Crittenden (1997), Kusumastuti et al. (2000, 2002), Satyana and Darwis (2001), Purwaningsih et al. (2002), Satyana (2002), Satyana and Purwaningsih (2002, 2003), Triyana et al. (2007), White et al. (2007), Van Simaeys et al. (2011) Hydrocarbons Java Sea: Kenyon (1977), Phillips et al. (1991), Matthews and Bransden (1995), Reynolds (1995), Kaldi et al. (1999), Mudjiono and Pireno (2002), Johansen (2003, 2005), Carter et al. (2005), Takano et al. (2008) S Java forearc: Bolliger and De Ruiter (1975), Lehner et al. (1983), Masson et al. (1990), Kopp et al. (2002), Schluter et al. (2002), Yulianto et al. (2007), Shulgin et al. (2011), Deighton et al. (2011) W Java Gold: Marcoux et al. (1993, 1996), Marcoux and Milesi (1994), Milesi et al. (1994, 1999) Bibliography of Indonesia Geology, Ed. 6.0 3 www.vangorselslist.com Sept 2016 Neogen di daerah Pacitan dan sekitarnya. Purwanto (2003). Indon. (online at: http://jurnal. M.pdf) ('Identification of the Karangtengah ancient volcano in the Southern Mountains.clastics series. hidrocarbon hunting in East Java Basin..6 m thick.id/dmdocuments/jurnal20090403. Four trends: NW-SE (~N320°E.unpad. R. 2012-GD-31. JAVA. Ito (2013). Wonogiri. (UNPAD) 13. Y. Java . Lower part is siliciclastic succession. M. Normal seismicity near trench low. Sapiie (2012). Bull. Suparka. 140-480 m wide and 0.S. greywacke. dip of 12°. Jawa Tengah. and part of volcanic island arc) Abdul. NE-SW (~N045°E.. (Structural analysis of faults in Pacitan area.ac. Harijoko & A. (UNPAD) 12.Identifikasi gunung api purba Karangtengah di Pegunungan Selatan. MADURA. Bull. E Miocene). A.The role of slump scars in slope channel initiation: a case study from the Miocene Jatiluhur Formation in the Bogor Trough. basaltic in composition. and dominated by normal faulting earthquakes in subducting plate. N-S. and probably source of carbonate detritus in upper part of Jatiluhur Fm (with Cycloclypeus annulatus)) Abdullah. Assoc. Scientific Contr. Wonogiri. with low 87Sr/86Sr and high 143Nd/144Nd ratios.. Joint Conv.III.id/bsc/article/view/8395/3905) (Jatiluhur Fm along Cipamingkis River. limestone. M. (Jatiluhur Fm. which formed on seafloor. JAVA SEA III. W Java. Hendratno (2009). Geophysical Research 106. M Miocene). Geol. K. W Java Middle. 68-86. M. onshore geology Abdissalam. 35A. part of M-L Miocene (N12-N16) clastic succession in Bogor Trough.A. S coast of East Java. Abdurrokhim & Hendarmawan (2014).Temporal variation in petrographic features of the Miocene Jatiluhur Formation in the Bogor Trough. Late Miocene Klapanunggal Fm = Parigi Lst in north is reefal limestone buildup. 2. Yuwono & B. and E-W (N080°E)) Abdurrachman. 48-56.General.com Sept 2016 . Scientific Contr. 41st Ann. Asian Earth Sci.S. Conv. Slump-scars-fill deposits have lenticular geometry. West Java. Proc. B4. p. Ed. Proc. Papandayan volcano comprises medium-K series with high 87Sr/ 86Sr and low 143Nd/ 144Nd. 107-117. 4. Geologi Indonesia 4.Between reality and illusion. up to 1000m thick in study area.esdm. Increase in volcanic fragments in Late Miocene suggests also sediment from contemporaneous volcanic provenances to S) Abdurrokhim & M. Sopandi (2005).vangorselslist. and interpreted as prograding slope-shelf system. located at Cretaceous suture zone. p. Cikuray volcanics low-K series. p.Analisis dinamik tegasan purba pada satuan batuan Paleogen.Limestone beds development of the Middle-Late Miocene Jatiluhur Formation in the Bogor Trough. Provinsi Jawa Timur ditinjau dari studi sesar minor dan kekar tektonik. epicenter depth 16km. West Java. (M-L Miocene Jatiluhur Fm in N Bogor Trough NE of Bogor feldspathic arenite. and mixed siliciclastic-carbonate. West Java.I. 253-267. Derived mainly from continental source in N (Sundaland).30th HAGI. Surabaya 2005.. ITB Journal Science and Technology.The 1994 Java tsunami earthquake: slip over a subducting seamount. West Java: a window into the past magmatism and tectonic event. M. 13p. which is locked patch in otherwise decoupled subduction zone) Bibliography of Indonesia Geology. Antolik.go.. Identification of E Miocene Karangtengah paleovolcano eruptive center. Yogyakarta. perhaps of missing 'Argoland') Abercrombie. E.4-1.Late Miocene (~N12-N16?) mixed limestone.1. (online at: www. Irfan & T. Felzer & G. N. Some slump scars formed incipient seabed irregularities that may have played important role in development of slope channels) Abdurrokhim & Hendarmawan (2015). J. S.Sr-Nd isotopic study of Papandayan area. p.0 4 www. 111-127. 7p. Magetsari & H. J. (IAGI). 2. C Java'. p. Ekstrom (2001). Interpreted as slip over subducting seamount. (First recorded large shallow thrust earthquake in South Java subduction zone. 73. 6. 107-118. (Sr-Nd isotopic ratios of young volcanics of Papandayan and nearby Cikuray (to E) volcanoes. Yamamoto. 2. p. with slump deposits and formed in slope and shelf-margin environments. Contrasting isotopic ratios explained by mixing of mantle wedge with Australian granites at Papandayan. J. Bronto. 34th IAGI. C. R.bgl. H. Lembang and Baribis fault zones have horizontal displacements of ~1-2 cm/yr.Z. F. A. Poor seismic imaging due to volcanic cover and rugged topography. corals (11 species) and calcareous algae (incl.M Zainal & Y. Novianti (2002). 15-20. 1. Geol. foram zones SBZ3/ SBZ4). 1707-1. with folded Late Oligocene-Miocene volcanics. Bibliography of Indonesia Geology. 28th Ann.Abidin. J.000. One target is Batu Raja Limestone. p. NE Java basin) Adhidjaja. p. Natawidjaya & H. 1-11..vangorselslist. 31-43 (Jatiluhur Block covers Bogor Trough and volcanic centers in S. 275-284. Isotopes suggest gold deposit formed due to mixing of magmatic ore fluid with meteoric water) Abidin.. J. T. IPA10-G-207. Bonn. West Java. Overlain by E Miocene sediments of Jaten Fm. 6. Post-seismic horizontal deformation of July 2006 S Java tsunami earthquake in first year after earthquake <5 cm. & S. Jakarta. 2nd Ann..000. 1. Andreas. (SE tip of East Java. Abdullah (2009). p. Jawa. M. decreasing after that) Abidin. One prospect is probable Batu Raja reefal buildup on basement high) Adinegoro. J. Di Carlo. Conv. Jakarta. I. (Low sulfidation epithermal gold deposit in Pengalengan District.M. Ed. 4. T. Russo (2010). including huge Jatibungkus limestone olistolith.Kemandung Ridges play concept to increase exploration prospectivity in East Tuban Block: preliminary study. West Java. (IPA). Miscellanea. Earthquake and Tsunami 3. J.PSDM Enhances reef interpretation in Jatiluhur Block. Pre-stack depth migration (PSDM) improved imaging. H. West Java. Distichoplax biserialis) suggest Late Paleocene age (Thanetian.J. rotaliids and discocyclinids). (IPA). Indon.H.. Davidoff & I. with potential overlying Ngimbang or Kujung Fm carbonate build-ups. A. associated with complicated structures. with best reservoir quality in buildup facies and typically developed on basement highs. tuffaceous sandstones and limestone of Batuampar Fm. Res. 34th Ann. Jakarta. Gamal. Achdan. (IPA). 2.com/abstracts/Accordi_etal_Jatibunkus_2010. Jawa. A. scale 1:100. R. Ilmu Kebumian Tekn. Majalah Geologi Indonesia 19.Z.Z.I. Symposium on Foraminifera. Bambang (2004). 77-88. & Baharuddin (2005). Dev. Meilano. Proc. (Pongkor low sulfidation epithermal gold deposit 80km SW of Jakarta. p. Hirosiadi (2010).Geological map of the Blambangan Quadrangle. F.girmm. (Poster Abstract) (online at: www. Centre (GRDC). Geol. Conv. Bachri (1993). Larger forams (Ranikothalia. in Tuban Block. Bandung. H.0 5 www.Reef limestone in the Sukabumi area. I.Z. intruded by Miocene andesites and granodiorites (= 'Old Andesites'. Quadrangle 1209-6. Indonesia.. Forams 2010. Gold in quartz veins hosted in altered ‘Old Andesite Volcanics’) Abidin. Proc. Ito. Gumilar & C.pdf) (Eocene Karangsambung melange of C Java with exotic blocks. 7 p. Res. D. I. Conv.Geology of the Pamanukan Quadrangle. (Seismic reprocessing improves imaging of NE-SW trending basement high named Kemandung Ridge. Dev. 6p. p. Indon. Proc. Int. Three main depositional environments) Adiwiarta.R. Pignatti & A. Centre (GRDC).I. R. carbon and oxygen isotope study of the Pongkor gold deposit. J. Harjono (2009)Crustal deformation studies in Java (Indonesia) using GPS. Geologi Indonesia 4.Sulphur. Pengalengan area. & Soetrisno (1992). (GPS surveys in W Java show areas around Cimandiri. (On deformation caused by 2006 Yogyakarta earthquake from GPS data) Abidin. Indon. Kato. Bandung. HvG). Petroleum Assoc. H. Kimata.. C Java May 2006 Yogyakarta earthquakes caused by sinistral movement of Opak fault with horizontal co-seismic deformation generally <10 cm.Deformasi koseismik dan pascaseismik gempa Yogyakarta 2006 dari hasil Survei GPS. H. Permanadewi & W. Petroleum Assoc. S of Regency (near Malabar Tea plantation?).Z.com Sept 2016 . Matteucci. U.Biostratigraphy of the Jatibungkus olistolith (Central Java).Low sulfidation epithermal gold deposit at Cibaliung Creek. H. M. and M Miocene Wuni and Punung Fms and Quaternary volcanics) Accordi. (1973). p. Carbone. Mineral 18. Petroleum Assoc. 109-120. 1:100. G. Andreas. H. Meilano. in Miocene host rocks. S. 1. J. Programs E and SE Asia (CCOP). Sukabumi. 279-298.Foraminifera of the Miocene Jatiluhur Formation: implications for the Indonesian Letter Classification and the planktic zonation scheme.Analysis and interpretation of seismic data from thin reservoirs. Coleman (1983). Prasetyo (1998). Talang Akar. September 1976. (Seismic amplitude analysis of M Miocene Parigi Fm carbonate reefs in onshore NW Java basin) Adriansyah. Open marine Cimandiri Fm S and SW of Sukabumi. Bandung. 20th Ann.Jatibarang sub basin. then terminating with carbonate sedimentation.J. U Cibulakan and Parigi Fms). Geophysics 66. SW Java. p. 1. Centre (GRDC). Sukabumi. 37-55. each initially filling with clastics. Northwest Java basin. 744-754. Not much detail on sample positions) Adisaputra-Sudinta. Jakarta. peripheroronda. (Jatibarang sub-basin in E part of NW Java Basin with oil-gas in E Oligocene. Miogypsina cushmani appears at base N9.AVA analysis and interpretation of a carbonate reservoir. W. Res. larger foram zone Lower Te with Heterostegina borneensis. 45. With seismic lines. 1.A. Bull. 3.Late-Miocene reservoirs (Jatibarang. 14-26. Dev. members. Adisaputra. with Glorotalia fohsi and Gr.(Study of Late Oligocene Rajamandala Limestone around Sukabumi. May be reworked into Pliocene. ~130m thick and divided into Bojonglopang. (incl. p. p.K. Spriroclypeus. Jakarta.Pleistocene deep water sediments from nearby uplifted fault blocks. Planktonics of zone N11-N12.N14). (M Miocene Jatiluhur Fm with larger foraminifera Katacycloclypeus annulatus (Tf1-2) in lower part and Lepidocyclina spp. Carbonate Seminar.K. Smit & E. van Vessem (1978). Centre (GRDC).earliest Miocene) Adisaputra-Sudinta. p. Central West Java. Java. & Arpandi (1976).in upper part. Indon. J. Top Miogypsina and Base Alveolinella quoyi near base N12. Miogypsina present in N8. at top Te5. 2-11.Biostratigrafi Formasi Cimandiri. (IPA).. etc. & H. Petroleum Assoc.K. with both planktonics (zones N2-N4) and larger forams (mainly Te1-4. McMechan (2002). Sub-basin formed in E Tertiary with formation of half-graben.Guide book fieldtrip to Sukabumi and Padalarang area. A. Lepidocyclina rutteni in N14) Adisaputra. (IPA). p.0 6 www. Indonesia. Miogypsinoides spp. 21-26.s. (Early Miocene shallow water limestone samples with Miogypsina-Miogypsinoides dredged from sites D1 and D2 (1500 and 2100 m) in Bali-Flores Basin. A. Sukowitono & Supriyanto (1991). U. 29-47. x-sections) Adriansyah. (1989).) Adinegoro. Nyalinding and Cimandiri s. p. L. Riset Geologi Pertambangan (LIPI) 9. Hydrocarbons controlled by presence of normal faults which provided vertical migration for hydrocarbon sourced from Talang Akar Fm. p. Sess. N of Sumbawa. Techn. Co-ord. Planktonic foraminifera suggest age mainly M Miocene (N8 (with Preorbulina glomerosa). & Budiman (1995). M. & G. Repts. Indon. Ed. & P. 22-34. NE Java: (1) Miogypsina cushmani in Middle Rembang Beds below Ngrayong-equivalent quartz sands.L. Conv. 34th Sess. Taejon. Bandung. Boundary between Tf1-2 and Tf3 lies within N11-N12) Adisaputra. Proc. Seri Paleontologi 4. radiata).Foraminifera from dredged samples in Bali and Flores basins: implications for tectonic environment. & G. McMechan (2001). p. ('Biostratigraphy of the Cimandiri Formation in the Central Jampang area. Bibliography of Indonesia Geology. p. Geol. Two graben generation stages. Petroleum Assoc. R.A.K. M.vangorselslist. Geol. J. Comm. Publ.a half graben model in the onshore of Northwest Java.Correlation between larger benthonic and smaller planktonic foraminifera from the mid-Tertiary Rajamandala Formation. Coastal Offshore Geosc. Indonesia. berdasarkan foraminifera plangton dan foraminifera besar.com Sept 2016 .) Proc. M. Geologi Sumberdaya Mineral 5.Miogypsina cushmani and Miogypsina antillea from Jatirogo (East Java). Geophysics 67. based on planktonic and larger foraminifera'. Korea 1997. Dev. A. Age close to foram zone N4. Northwest Java basin. (Localities on Jatirogo Quadrangle. M. M. 2. Late Oligocene. 6. Rau (ed.K. probably equivalent of M Miocene ‘Platen Limestone’) Adnan. In: J. (Samples from Tagogapu/ Cikamuning part of Rajamandala Limestone in W Java.. and (2) Miogypsina antillea in 200m thick ‘U Rembang Fm/ Tlatah Limestone Beds'. di daerah Jampang Tengah. Res. Gradual δ18O increase (cooling) in Late Miocene (~12 Ma) in all taxa can be correlated to global cooling and/or closing of Indonesian seaway. p. D. p. In: Proc. Bandung. Ed. Ardhito (2014). (IAGI).New interpretation on magmatic belts evolution during the Neogene. ('Biostratigraphy of nannofosils in the Oyo Formation along the road of Gunung Lanang.A. Indon. K. Indon. due to closure of Indonesian seaway.Geological and tectonic implications obtained from first seismic activity investigation around Lembang fault. (Incl. Bayat. 97-102.pdf) (Microseismic events around Lembang fault at N side of Bandung suggest this fault is left-lateral fault) Agnes M. (IAGI). Old Ijen.(Attribute analysis. Central Java. 1708-1. Jakarta. Rahardjo (2000). 6th Int. 43rd Ann. Akmaluddin. suggesting Oyo Fm is of Middle -Late Miocene age. A. Watanabe (2009). Watanabe (2012). p. S Mountains SE of Yogya. S Mountains. 4. K. Watanabe (2009). Seminar on Geology of the Southern Mountains of Java. Indonesia. Yogyakarta.The characteristics of foraminifera distribution patterns within turbidite sequence of Banyak Formation. Akmaluddin & Y. Geol. daerah BayatKlaten. 247-252. which moved to presentday location in W Pacific after ~10Ma. Klaten area'.vangorselslist. 2. Buletin Geologi (ITB) 32. 235-238. Itaya (2005). 41st Ann. 6. (online at: www. In: Proc. Assoc. PIT IAGI 2014-247. 1-9. Kamei & K.. Int. Low δ18O values (warming of bottom water) of benthic foraminifera at ~18 Ma and ~12 Ma.) Akmaluddin (2008). Dev.1186/s40562-015-0020-5.Biostratigrafi nanofosil Formasi Oyo jalur Gunung Lanang. 1. impedance inversion and full-wavefield modeling of 2-D seismic line over thin gas reservoirs in E-M Miocene U Cibulakan Fm clastics in NW Java Basin suggest reservoirs detectable even when less than tuning thickness) Afnimar. NN8 (Catinaster coalitus). C Java. Assoc. Kano & K. 34th Ann.Geological map of the Situbondo Quadrangle. Yogyakarta. Central Java-Indonesia. Akmaluddin. Geol. overlain by Quaternary volcanics of Ringgit. Workshop on Earth Science and Technology. D. Indonesia. In: Proc. 103-108. Setijadji.L. & S. A. Geol. Yulianto & Rasmid (2015). etc. Calcareous nannofossils Gn Lanang four zones: NN 7 (Zone Discoaster exilis).0 7 www.000. 1992 geological map)) Akmaluddin. Agustiyanto. 5p. Conv. Surabaya. Raung. with folded (Late) Miocene. p. Yogyakarta 2009. Baluran. 2012-SS-10. p. Watanabe & T. Maryunani & A. Central Java. Int. Geol. 1. Proc. and hornblenderich tuff of ~12 Ma) Bibliography of Indonesia Geology.Pliocene sediments. Low planktonic δ18O values indicate sea surface T in this area higher than other tropical areas during E-M Miocene. (NE-most tip of Java. comparable to N13-N16 zone of planktonic foraminifera (younger than N8-N11 age suggested by use of foraminifera in Surono et al. Indonesia.com Sept 2016 . Decreasing of carbon δ13C in Late Miocene likely correlates to 'carbonate crash'. probably related to development of W Pacific Warm Pool. DOI 10.Quaternary periods as revealed from newly-collected K-Ar ages from Central-East Java. Yogyakarta 2009. A. Centre (GRDC). Proc.Preliminary study of high-resolution correlation and calibration of biodatum marine microfossils (foraminifera and nannofossils) using strontium isotope stratigraphy: case study in Southern Mountains.com/content/pdf/s40562-015-0020-5. Late Miocene-Pliocene K-Ar age of diorite in Selogiri area. Proc. Kano & K. scale 1:100. E. 1. Indonesia.Paleoclimate reconstruction based on oxygen isotope composition of foraminifera in Southern Mountains area. (IAGI). NN9 (Discoaster hamatus) and NN10 (Discoaster calcaris). Assoc.Age correlation of Oyo Formation based on nannofossils and foraminifera biostratigraphy at Southern Mountains area. Seminar on Geology of the Southern Mountains of Java.A. (Oxygen isotopes study of planktonic and benthic foraminifera from Ngalang River section.geoscienceletters. Conv. Jawa.Paleoceanography of Central Java and closing of Indonesian Seaway reconstruction based on oxygen isotope composition of foraminifera. Santosa (1993). p. Indon. Res. 1-11. p. Geoscience Lett. Conv. at ~11-10Ma) Akmaluddin.T. 71. Rahardjo (2012). Universitas Gadjah Mada.Oligocene-Early Miocene foraminifera. C Java.Miocene calcareous nannofossils and foraminifera biostratigraphy. Kano & W. Epidoteglaucophane schist. Technology. Results indicate gap between Sambipitu and Oyo Fms. In: E. Proc. West Java: a fluid inclusion and geochemical study. Sloane & T. 6. Conv. 40Ar/39Ar date of 10. Sudharto (1994). Assoc. Sambipitu Fm 5 zones (NN2-NN6. Results suggest gap between Sambipitu and Oyo Fms. Proc. Pros. R. Conv.vangorselslist. tied to Late Miocene global cooling or due to closing of Indonesian Gateway) Akmaluddin. Brennan (ed. with absence of NN7.0 8 www. (IAGI). Warming of sea surface T related to development of W Pacific Warm Pool and flow of warm water through Indonesian seaway. p. 1p.Calcareous nannofossils biostratigraphy of Ngalang River section. J.org/journals/waset/v71/v71-11. Conv.F. Metamorphic rocks in Jiwo Hills mica-albite phyllite.I. Foraminifera biostratigraphy of Sambipitu Fm 4 zones (N6N8a). 25-38. good agreement with nannofossil biozones. Indon Geol. D. Java'. Suggesting younger ages than dated previously) Akmaluddin. hosted by Miocene monzodiorite stock) Alderton.M. hamatus (9.Mineralization at Gunung Limbung. T.3 Ma of Oyo Fm tuff layers in agreement with biostratigraphic ages (tuff layers 10m above FO Discoaster hamatus (10. Oyo Fm 3 zones (NN8-NN10. (On base metal mineralization at Gunung Limbung in several steeply-dipping quartz veins. E. Klaten regency. M. & R.Sambipitu Fms. p. Geol. 19. 1 p. Assoc. Sambipitu Fm shows 5 zones (NN2-NN6. Central Java. near Top Globigerina binaiensis) Akmaluddin. D. 41st Ann.) Proc. Yogyakarta. Yogyakarta. gabbro and serpentinite may indicate Cretaceous subduction process and presence of ocean plate stratigraphy in Jiwo hills) Bibliography of Indonesia Geology. 5-8. Ohira (2012). R. Metamorphic protoliths mainly pelitic sediments. Cooling at ~12 Ma. demonstrate warm sea surface T during Miocene..2 Ma. Bayat. inconsistent with nannofossils. Proc. (Abstract only) (Fission track dating of 3 samples from lower.M Miocene). 20m below LO D. K. quartzite. E-M Miocene). Harmon. Watanabe.L Miocene). Yogyakarta.waset. (IAGI). 35th Ann. Decrease of O isotope values at ~14 Ma. glaucophane marble with lawsonite. K.8±1. 1 p.Miocene warm tropical climate: evidence based on oxygen isotope in Central Java. Watanabe & W. but also basaltic-andesitic rocks. serpentinite. calc-silicate schist. M-L Miocene). near FO Globoquadrina dehiscens. S Mountains. Ed. C Java. Parkville. 2012-SS-09. Susilo & W. A. Asian Earth Sci. graphite schist. Southern Mountain area.com Sept 2016 . p. middle and upper Semilir Fm at Buyutan section yielded ages of 23.7 Ma) and FO Globigerina nepenthes (11. Assoc. of Mining and Metallurgy (AusIMM). tied to M Miocene Optimum. Seminar Nasional KebumianKE-7. Setiawan (2014).H. 40Ar/39Ar dating & fission track dating in Southern Mountains. p. Indon.pdf) (O and C isotopes records of foraminifera and bulk carbonates from Oyo. marble. West Java. Pacific Rim Congress 1987. (Abstract only) (Calcareous nannofossil analysis on Miocene Sambipitu and Oyo Fms at Kali Ngalang section.0±1.4 Ma. S Mountains. Jurusan Teknik Geologi. Engin. Kabupaten Klaten. Oyo Fm 3 zones (NN8-NN10. 66-70. Provinsi Jawa Tengah.Fluid inclusion and stable isotope studies at Gunung Limbung Cu/Pb/ Zn deposit. Australasian Inst. World Academy of Science. (online at: www.7 Ma). Watanabe & H.Akmaluddin.4 Ma)) Alderton. Gold Coast. K. 10. Central Java. & N. garnet-wollastonite skarn and metasiltstone. 40km W of Bogor) Alfyan. Geol. but M Miocene (Oyo Fm) suggest hiatus of N10-N12. epidote-glaucophane schist.T. Pekanbaru 2006. Indonesia. albite-mica schist. (IAGI).Petrogenesis batuan metamorf di daerah perbukitan Jiwo. Indon. Yogyakarta. with calibrating the age using 40Ar/39Ar dating in Southern Mountains. (Cu-Pb-Zn sulphide mineralization associated with M-U Miocene quartz monzonite stock. (Abstract only) (Samples from Miocene Sambipitu and Oyo Fms of Ngalang River section. Gunung Kidul.5 Ma and 19. Sudharto (1987). 2012-SS-08. Kecamatan Bayat. Rahardjo (2010). gabbro. Rahardjo (2006). 41st Ann. (Abstract only?) ('Petrogenesis of metamorphic rocks in the Jiwo hills. M. Indon. p. IPA11-SG-015. Anonymous (1922). 41st Ann. (IAGI). 1-40. IPA11-SG-020. Conv. East Java. Nglipar Area. S part of NE Java Basin.. Proc.G. Indon. Dienst Mijnbouw Nederl. At least four types of play: facies change. Indon. based on gravity data.M.Geology study Malingping area. T. & Exhib.A. Indonesia. p.. 4. Yogyakarta: an explanation for the dynamic process of volcaniclastic turbidite Sambipitu Formation in Java Oligo-Miocene volcanic arc.D. (Cibaliung gold project in SW Java. Fahlevi. W of Bajah Dome.Geology and alteration-mineralization characteristics of the Cibaliung epithermal gold deposit.Play identification for Paleogene rift sediment in Ngimbang Sub Basin.Ichnofacies study of volcaniclastic turbidite Sambipitu Formation based on outcrop data in Ngalang River. 14. Petroleum Assoc. Oost-Indie. Joint 36th HAGI and 40th IAGI Ann. p. 10th Ann.. Bachri (1992).P. P054. Bibliography of Indonesia Geology. Res.. Nahrowi. 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Hydrothermal system responsible for mineralization may be related to rhyolitic magmatism near volcanic intrusive center during back arc rifting that formed graben or pull-apart basin (see also Harijoko et al.Contribution of organic petrography study on organic-rich sediment to the depositional environment determination of Upper Semilir Formation of Southern Mountain in Yogyakarta. Proc. 6.. JCM2011-215. Cekungan Jawa Timur bagian Utara. T. Dev.. (IPA). 21st Ann. Ed. scale 1:100. Indon. Indon. 463-476. Noeradi. Iswandi (2011). 8p. Assoc. Hardito. 35th Ann. Tambunan (1992). intruded by andesite-diorite plugs and dykes. In: 74th EAGE Conf. Octaviani & B. interpreted as lagoonal-estuarine facies) Aminuddin. basin floor fan and channel fill plays) Anom. Jakarta. S. ('Study of the Selorejo Formation. Kartika & M. 2. 0-50m in S. Geol. L. A. (IAGI). R. R. B.. Akbar & S. Situbondo Area. Conv. Conv. Ubaidillah (2011). Proc. Angeles. NE Java'. (IPA). Purnamasi. alluvial fan. 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(Pre-Eocene meta-conglomerates from Jiwo Hills with clasts of poorly sorted sandstones and volcanics and common chromian spinel grains derived from mantle peridotites. Ngrayong Sst Fm generally age N9-N10) Apotria. Millman (2009). Age. (Online at: http://journal. Noda & K. (online at: www. Central Java. p. (2007). (online at: http://jrisetgeotam.com/index. Petroleum Assoc.Metamorphic and related rocks from Jiwo hills near Yogyakarta. peridotite or chert. (On detrital carbonate aprons around Oligo-Miocene buildups in Cepu Block. Yamagata University.Detrital chromian spinels of fore-arc mantle origin in meta-conglomerate from a preTertiary metamorphic complex of Jiwo Hills. Several basaltic volcanic rocks at Karangsambung melange complex. is opal-CT.0 10 www. 151-170. sulfur. etc. Unlike conclusions of earlier workers on Java there are potentially commercial gold-siver-copper mineralizations in Jampang area SW of Sukabumi. 6. Karangsambung.('Results of mining-geological surveys in the Jampangs. Conglomerate possibly fill of Marianas-type trench. as penetrated by Jambaran 2) Aoki. Dienst Mijnbouw Nederlandsch-Indie. Walley. Indon. & N. (IPA).php?li=article_detail&id=645) ('Foraminifera distribution patterns within sequence stratigraphy. p. 278-279. S. SW Java. Jakarta. 1-9.) Micropaleontology. A. Marked subsidence observed to W of. Geochemistry analysis suggest silica-saturated basalt of tholeiitic normal mid oceanic ridge basalt (NMORB)) Ansori. Derewetzky & D. berdasarkan analisis geokimia. quartz sand. 3.Model mineralisasi pembentukan opal Banten. where peridotites were exposed and sediments and volcanics were supplied from arc) Arai. 1-87.Pleistocene folding. kolen en ertsen. Riset Geologi Pertambangan (LIPI) 17. 7-14. in quartz veins associated with igneous intrusives) Anonymous (1939). Review of occurrences of gas. east Java. Weidmer. 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(IPA). lower shoreface) and (3) Zoophycos-Chondrites (offshore shelf. Zaim. (Brief discussion of Late Miocene potential reservoirs in N Serayu Basin. In Neogene volcanic belt moved N to N of Bogor Through.go. suggesting fore-arc basin. 15-23. Thesis UNPAD University.Karakteristik fasies sedimen Paleogen.Neogene sedimentary facies of C Serayu Basin. 1.Oligocene was part of Bogor Trough/ Bobotsari Low. Volcanic detritus and abundant feldspars in most samples from M-L Eocene-Oligocene Worowari Fm suggest main source is from volcanic rock. Kalibiuk Fms) in N19-N20 (E-M Pliocene). S. 4.Batuan asal dan alas formasi Paleogen Cekungan Seraya. C Java.Seismic identification and characterization of gas hydrates in Central Sunda margin. Gradual shallowing to coastal environment (Tapak. (2014). (2012). which was subsequently eroded. Hakiki. p.Pengaruh tektonik regional terhadap pola struktur dan tektonik Pulau Jawa. Purbalingga Regency. but supposed to be deposited. Low bounded by S Serayu Range high in S. Late Miocene turn to deep marine environment. E-M Miocene trangression. Paleocurrents indicates S-SE ward transport direction. End Oligocene inversion formed mountainous area. Early Neogene sediments suggest increasing tectonic activity followed by increasing volcanic activity from older unit to younger rock units) Bachri. sandstones and include Nummulites limestones) Bahar. p. J. Turbidites at base with abundant radiolaria and deep water benthic forams (Bathysiphon. Bachri.Bachri. ('Provenance and basement of the Paleogene formation in the Serayu Basin'. A. with peak volcanic activity as suggested by Kumbang Volcanics. Bordered in S by high of S Serayu Range. (2011).com Sept 2016 . develop into olistostrome of claystone matrix with blocks up to 10s of m. in back-arc basin. Sumber Daya Geologi 20.S Sumatra)) Baharuddin & S.D. 6. Surachman (2006). Peak volcanism in Late Miocene. 199-208. p. (online at: http://kiosk.geology. 215-221. S. Based on residual gravity map Bobotsari Low represents ENE-WSW trending graben. Widiyantoro & Y. Permanadewi (2012). 8th SEGJ Int. p. New name Worawari Fm for M Eocene. p. ('The effect of regional tectonics on the structural pattern and tectonics of Java island'. which during M Eocene. J. Geologi Sumberdaya Mineral 15. and polymict conglomerates.Indikasi batuan adakitik di Pacitan. but also metamorphic slate fragments and quartz-rich rocks.0 14 www. Santoso.vangorselslist. 6. 4 (203). p. 25-32. probably part of Sunda Platform) Bachri. S. 4. (2011). p. J.Neogen Cekungan Serayu sebagai respon atas kegiatan tektonik dan vulkanisme. Jawa Timur. (Significant hydrate accumulation interpreted from Bottom Simulating Reflector on BGR seismic lines in central Sunda margin (forearc region off SW Java. (2010). Sumber Daya Geologi 22. Central Java. Kyoto 2006.. Ph.Pengaruh kegiatan tektonik dan gunung api terhadap karakteristik sedimentologi sedimen Neogen awal daerah bagian tengah Cekungan Serayu. D. Paleogene change in structural trend from NE-SW to E-W) Bachri. C Java.earliest Pliocene (Kumbang volcanics)) Bachri. Sumber Daya Geologi 21.esdm. Bibliography of Indonesia Geology. C Java. Sumber Daya Geologi 20. J. J. J. S. In: Proc. p.id/artikel/pdf/sedimentologi-formasi-worawari-paleogen-dipegunungan-serayu-utara) ('Sedimentology of the Paleogene Worawari Fm in the North Serayu Mountains'. Detrital zircons suggest Late Cretaceous basement age (~68 ± 9 Ma). (Unpublished) (On Paleogene.Basin development and Neogene deposition history in Bobotsari Low. (Bobotsari Low is part of Bogor Through in Purbalingga area. S. Sumber Daya Geologi 22. 209-215. & H. F. S. 1-5. Paleogene not exposed. Symposium. (The influence of tectonic and volcanic activity on the sedimentological characteristics of Early Neogene sediment area of the central part of the Serayu Basin'. During Late Paleogene C and W parts of Java and Java Sea magmatically inactive or stable. In distal environment turbidites of Penyatan Fm formed. Cyclammina).Oligocene deep marine turbidites and olistostrome deposits ENE and NW of Banjarnegara.Indonesia. Panggabean (2010). 1.Sedimentologi Formasi Worawari Paleogen di Pegunungan Serayu Utara. S. 285-292. Ed. ) Basuki. Bull. Indonesia: In: 11th Reg. 10 km NW of Pelabuhan Ratu.('Indications of adakitic rocks in Pacitan. p.ac. In: N.. Malaysia 43. Harijoko & K. followed by extension since Pleistocene. East Java'. (online at: http://jgi.com/2014/09/bgsm1999025. J.Diagenetic pattern in the Citarate carbonate rocks.ugm. Kuala Lumpur. 69. In: T.php/JGI/article/view/30/22) (E Miocene Citarate Fm in Cilograng. 2. 2.Oligocene. Kuncoro & K. Indonesia. D.E Miocene 'Old Andesite' and Cimapag Fm volcanics. A. S. Watanabe (2010). K/Ar dates of mineralization 8-9 Ma.. Soc. A. hosted in Late Oligocene. Geology and Mining (NIGM) 5. 2012.H. Conf.pdf) (Yogyakarta region. Indonesia.. Sunarya (1999).ft. Malang. Mineral and Energy Resources of Southeast Asia (GEOSEA 2009). Suparka (2012). E. Basuki (ed. Age of mineralization probably same as at Pongkor. Congress Geology. Barianto. Aboud & L. West Java. 371-391. Cilograng Area.pdf) (Epithermal gold deposit at NE side of Bayah Domein in SW Java. Banten Province. Prihatmoko & E.I. Indonesia.Gold deposit in the Cikidang area. central part <120m.id/index. p.A. & S. gravity data. 85-100. Yogyakarta. Yb) Barianto. NE-SW-trending central depression bordered by two parallel faults. Southeast Asian Applied Geol. p. E. Pliocene uplift after deposition of Kepek and U Sentolo marls. Geol. Nat. Ed. Two major faults divide area into three parts. 13-28. W part uplifted >590m.com Sept 2016 . 65-77.A petrographic study on diagenesis of reef-associated Rajamandala carbonate rocks.pdf) (Development of NE-SW trending Yogyakarta graben. where dated as 2. depression and bordering blocks were in same depositional environment (inner neritic) during N9 (M Miocene). Geologi Indonesia 7. E part uplifted above 170-300m) Barianto. Fac. p. (online at: http://geologic-risk. 1. D. (online at: http://pustaka.A. 9th Reg. associated with Neogene calc-alkaline volcanism. Foraminifera suggest all blocks in shallow marine environment in zone N9 (~15 Ma). Indonesian Soc. Geol..) Proc. Congress Geology.E Miocene 'Old Andesites' volcanic and intrusive rocks from Pacitan area in Southern Mountains basaltic -andesite to rhyolite. Present positions indicate W part uplifted higher than others (>590 m). Sumanagara & D. Geochemical Exploration 50.kyushu-u. West Java. displays 9 phases of diagenetic events. Kuala Lumpur 1998..The use of foraminifera fossils for reconstructing the Yogyakarta graben. Kyushu University. p.vangorselslist. C Java. Teh (ed. Setijadji (2009). 3. D.Gold mineralization systems in Southern Mountain Range. Mem.H.M. (MGEI) Ann. In: G. Inst. (1975). In: Proc. P. Indonesia.H. Padalarang area. 137-144.I.pdf) Bibliography of Indonesia Geology. Central part uplifted <120 mm. (eds.H. D. N. Several samples adakite-like.I..lipi.jp/dspace/bitstream/2324/14900/1/paper4. (online at: https://qir.. Different uplift rates created depressed block between two faults. with high Sr and low Y. p. Suparka & Y. Lebak Regency.esdm. 138-143.1.bgl.id/wp-content/uploads/2016/02/NIGM-5-1. and paleontological data from Tertiary rocks in Yogyakarta.The Tertiary volcanic rocks distribution in Yogyakarta and its vicinity. p.files. (Gunung Pongkor gold-silver deposit in W Java several steeply dipping epithermal quartz-veins. N. Manila 2009. Associated with Plio-Pleistocene intrusion. P.The Middle Miocene diastrophism: its influence on the sedimentary and faunal distribution of Java and the Java Sea Basin.I. N.The Gunung Pongkor gold-silver deposit. Indonesia. (https://gsmpubl. Watanabe (2009). of island arc affinity.0 15 www.) Indonesian mineral deposits. Wiyoga (2012). p. 251-259. Bull.1. West Java. J. Sinambela (1994). Banda and Eastern Sunda arcs.Structural analysis using Landsat TM.go. van Leeuwen et al.go.id/fresh/jsaag/vol-2/no-2/jsaag-v2n2p138. A. J.5 Ma) Basuki. (2009).D. Production started in 1994) Basuki. Earth Science Int. Baumann. (UGM) 2. E part >170-300m) Basuki. Engineering. Conv. Based on foraminifera observations. Mineral and Energy Resources of SE Asia (GEOSEA ’98).ac. 6.) Proc.geotek. West Java.Discoveries of the past 25 years. (Abstract only?) Basuki.wordpress. p. Econ. . Knott et al. 19. L. Petroleum Assoc. p. Ed. P. serpentine. 2nd Ann. P. A.) Petroleum Geology of Southeast Asia. augietandesieten.J. (4) M-Late Miocene.. Petroleum Assoc. Afd. (1943).).Depositional cycles on magmatic and back arcs: an example from Western Indonesia. basalt en tachylyt. p. (2001). with discovery of a new species of Solen and proposal of a new name for a Ptychocerithium species. Of 74 mollusc species. See also Soeria-Atmadja et al. S.Chronologie 40K-40Ar du volcanisme Tertiaire de Java Central (Indonesie): mise en evidence de deux episodes distincts de magmatisme d'arc. J.Fault seal analysis of SE Asian basins with examples from West Java. (On Eocene gastropod species Puruninella permodesta from Upper Eocene of Nanggulan. T. Priadi. Faunal composition and rapid diversification of larger foraminifera (species of Miogypsina. Soeria-Atmadja (1989). (1997).D. (5) PlioceneRecent) Baumann. (IPA). Conv. Maury & R. H. Brockbank. Geologie en Mijnbouw 5. p. ('The species Buccinulum in the Early Miocene of the island Madura') Behrens. Proc. In NE Java basin Ngrayong sandstones unconformably overlie Upper Orbitoiden Limestone (OK). (Summary of geology. 20. 309.C. Natuurkunde. In: A..E Oligocene. Geologie en Mijnbouw. tachylyt and Tertiary conglomerates from the surroundings of Ciletuh Bay'. Mudjito & S. Bazzacco. augite andesites. p. Spec. Beets. Indonesia). p. B.E Miocene. Murphy (eds. Polve. 185-194. p.com Sept 2016 . Samuel. M. while 35 others have affinities with European Eocene species) Beach.(Widespread evidence of M Miocene deformation and regression across much of Indonesia. Proc. Publ.J.Contribution to the geological knowledge of Southwest Java. I.. C. P.Pliocene (11-3 Ma) (initiation of modern Sunda arc). Suminta & Wibisono (1972).. (1944). Conv.. 1994) Bibliography of Indonesia Geology.Uber Puruninella permodesta (Martin) aus dem javanischen Obereozan von Nanggulan. Fraser. de Genevraye. Two Tertiary subduction-related volcanic events in C Java: Eocene. Akademie Wetenschappen. Jakarta. H. n.H. 80p.The Cenozoic of Java and Sumatra. studied earlier by Boettger 1883 and Martin 1914. Francais Petrole 37. p.Beitrage zur Petrographie des Indischen Archipels.W.L. 1931. II. Oesterle. Soc.s. a hiatus spanning planktonic foram zones upper N9-lower N11. Verslagen Kon. 6. (Four main sedimentary cycles on Java-Sumatra-Sunda Shelf. Pringgoprawiro. Jakarta. Paris.J. Sajekti (1973).E Miocene (40-19 Ma) and late M Miocene. (Listings of M Eocene mollusc assemblages from Nanggulan. W of Yogyakarta. Brown. p. R. 126. Indon. basalts.H. Indon.0 16 www. 16 also found in other Tethys basins. 1971-1977. Padova. 53. ) Baumann. each starting with transgression and each ending with a phase of volcanism and tectonism: (1) M Eocene.Die gattung Buccinulum im Altmiozan der Insel Madura (O. (2) Late Oligocene. (3) E-M Miocene (missing in many places under M Miocene erosional surface. ('40K-40Ar chronology of the Tertiary volcanism in Central Java: evidence for two subduction-related magmatic events'. S. 29-35. rise of Barisan Mountains in Sumatra. Matthews & R. Amsterdam. P.-I. May also be time of overthrusting of allochthonous terranes of Timor. Comptes Rendus Academie Sciences. benevens tertiaire conglomeraten uit de omgeving der Tjiletoek-baai. (1982).Revision of a Middle Eocene mollusc assemblage of Nanggulan (Java. Lepidocyclina) may be response to fast changing environments. Revue Inst. (IPA). (1880). 14-16. 1. 31-42. M. C. C Java) Beets. 6. 105-108. Mikroskopische beschrijving van gabbro en serpentijn.vangorselslist. Geol. Memorie Scienze Geol.stratigraphy of SW Java) Baumann. 92-93. Ser. P. ('Microscopic descriptions of gabbro. 3-17. Not clear why gap in volcanism from 19-11 Ma. 1st Ann. One of first descriptions of rocks from SW Java melange complex) Bellon. H. Raninellopsis javana n. 6. Palaeontographica Suppl... No figures) Boachi.sp. Djokdjakarta. (1856). 6th Regional Conf. Natuurkundig Tijdschrift Nederlandsch-Indie 9. Proc. C.Die Mollusken der Oligocaenen Schichten vom Bawang-Flusse.Imaging fluid-related subduction processes beneath Central Java (Indonesia) using seismic attenuation tomography. Yogyakarta and Rembang) from collections of Verbeek and Martin.O. 2.Bellon.6.com Sept 2016 .0 17 www. Insel Java. (1883). 225-266. Wetenschappelijk Gedeelte. p. 1-83. H. Jaarboek Mijnwezen 1883. R. and Martinocarcinus ickeae n. Ed. L.M. 461-464. 49-52.Arthropoda.C. O. E. SW Java'. Suparka & Y. A.. Muria). p.Die Mollusken der Oligocaenen Schichten vom Bawang-Flusse. Residency Yogyakarta. ('Investigation of the coal found along the beach of Peucang Bay'. 32nd Ann.A geophysical study of the forearc region South of Java. Res. from Ci Lalang. p. ('The molluscs of the Oligocene beds of the Bawang River.sp. Java'. Residency Yogyakarta. Indonesia. A. Tectonophysics 590.sp. Ciletuh Bay partly surrounded by serpentine hills. (On Miocene-Pleistocene volcanism on Java Sea islands Bawean.repository. (IAGI) and 28th HAGI Ann. Nucia and Calianassa from E Miocene of W Progo. Prominent zone of increased attenuation below and N of modern volcanic arc down to 15 km related to EoceneMiocene Kendeng Basin. overlain by sandstone. One of few reports by African Prince/ mining engineer Akwasi Boachi. Karimunjaya and Java N coast (Lasem. Java Pleistocene volcanoes (1. Conv. Reichs-Museums Leiden (N. CA. (1856). II Theil. (= Early Miocene?. M. (1922). 10-11. U Eocene Scylia laevis n. Martin. Myra. Eclogae Geol. On occurrences of coal at far W point of Ujung Kulon Peninsula. Natuurkundig Tijdschrift Nederlandsch-Indie 11. facing Sunda Straits. J. from E Miocene of Rembang.. Neptunus from Nyalindung.) Boettger. H. IAGI.naturalis.M (1966). Yuwono (1989). p. S. See also Ngkoimani et al.F. R. HvG)) Boettger.D. Situmorang (ed.I. 1. Sammlungen Geol.nl/document/552452) (Eocene and Miocene crab fossils from Java (Priangan.The planktonic foraminifera in well Bodjonegoro-1 of Java. Helvetiae 59. (Earthquake data used to build 3-D image of seismic attenuation in crust and upper mantle beneath C Java.Chronology and petrology of back-arc volcanism in Java. Geology Mineral and Hydrocarbon Resources of Southeast Asia (GEOSEA VI). Reprint of Boettger (1883)) Bohm. p.Reconstructing Cenozoic Java using paleomagnetic data.sp. Residentie Preanger Regentschappen. p. 245-257. 2006) Boachi. 3. Incl. In: B. (1883). 125-148. Scyllarus junghuhni n. p. Master Thesis. 521-535. Molluscs from marls above andesite in North Serayu Mts. In: Die Fossilien von Java auf Grund einer Sammlung von Dr. Bibliography of Indonesia Geology. 3. (Abstract only.D. Callianassa frangens n. Maury. Djokdjakarta. C.S. Indon. etc. In: R. (1982). R. p. Soeria-Atmadja. p. (online at: www. Verbeek und von anderen bearbeitet durch Dr. Enhanced attenuation also in upper crust near recent volcanoes pointing towards zones of partial melts) Bolli.3 Ma) increasing K2O content away from trench) Benaron. Although unfossiliferous quartz sandstones present. (1883) Die Tertiarformation von Sumatra und ihre Thierreste. Verbeek et al. Abdullah & T. University of San Diego. no outcrops of coal were found) Boehm. Several thin layers of lignite in area with common petrified and coalified wood. Conv.0. Ngkoimani.) Proc. Java'. 175-188.Onderzoek naar het aanwezen van steenkolen in het terrein aan de Tjiletoekbaai.sp. K. Assoc. (Unpublished) Bijaksana. N. O. Jakarta 1987. ('The molluscs of the Oligocene beds of the Bawang River. Ungaran. Insel Java..vangorselslist. Hardjono (2003). Jakarta. ('Investigation of the presence of coal in the terrane on the Ciletuh Bay. Asch (2013). 449-465.M. Haberland & G. Res. 4p. Geol. from Kali Puru. Nanggulan.Onderzoek naar de kolen gevonden langs het strand van de Meeuwenbaai.) 1. Revue Paleobiologie.nl/DL/publications/PU00016873. Padova. Purwakarta and Bandung areas. Width of volcanic arc in W Java and Banten ~80-100km) Bronto. Both wells TD in pre-Miocene volcanic agglomerates and basalt) Boomgaart. (1929). 3. Bayah Pongkor.Merapi volcano and the Southern Mountains. M.Pliocene planktonic foram zonation in Indonesia. (‘West Java Tertiary volcanoes: identification and implications’. 1-14. Most of W Java and Banten areas covered by volcanoes and their products. Two dry wells in Miocene carbonate targets. Bothe. 1934).5169/seals-163383) (Classic study of E Miocene (G.A. Doct. S. Six groups distinguished. 291-309. (Unpublished) (Classic study of E Miocene.Smaller foraminifera from Bodjonegoro (Java). S Mountains of C Java.Significant Miocene larger foraminifera from South Central Java. insueta zone) to Pliocene (Gr. Ages of volcanoes Paleogene.com Sept 2016 .Geology of the South Central Java Offshore area.Smaller foraminifera from the marl zone between Sonde and Modjokerto (Java).(online at: http://dx. 2. Geneve. Lokier (2005).. G. Eocene-Oligocene volcanics more rare and widely scattered) Bronto. (Unpublished).knaw. (IPA). (online at: www. de Ruiter (1975).D. (2003). Fieldtrip Guidebook. (1934). University of Utrecht. Boudagher-Fadel.0 18 www. p. mostly close to South coast. Majalah Geol. p. p. Fifteen Mio-Pliocene volcanoes in central-northern part. (1971-1974 Shell work on South Java forearc basin exploration. W. Petroleum Assoc. 1. p. i. Amsterdam. 75-81. 1949. (Showed validity of the then new ‘global’ E Miocene. (2008). No location maps. See also comments by Renema (2006)) Braga. Bandung. S. Excursion Guide C1.C. Yogyakarta: volcanoclastic rocks for petroleum geologist.Tinjauan geologi gunung api Jawa Barat. p. Vroman (1947). HvG)) Bolliger. 48p. (1949).Djiwo Hills and Southern Range. 1175. Geol. roughly same zone as Quaternary belt. & J.Pliocene smaller benthic foraminifera in continuously cored Bojonegoro 1 well (BPM.Quaternary. & S. Jurnal Geoaplika 3.Gunungapi Tersier Jawa Barat: identifikasi dan impliksinya. Sheet Klaten.vangorselslist. Jakarta. W Java. indicating superimposed volcanic episodes. E Java. p.C. (M Miocene Tf1-Tf2 larger forams from Wonosari Fm in Gunung Sewu area. Ed.K. Java 1929. ('Overview of the volcanic geology of Banten. L. 1. p. rotalids. (2001). A..Occurrence of Cenozoic bryozoa in Nanggulan and elsewhere in the Indonesian Archipelago.D. W Java ten Oligo-Miocene volcanoes.Banten dan implikasinya. Nederl. Bibliography of Indonesia Geology.Pleistocene sediments from eastern Kendeng zone near Mojokerto.dwc. 2.org/10. Alveolina 1 with E-M Miocene carbonate section.doi. 24. 53.e. 39. Indonesia 18.Pliocene section is in bathyal facies) Boomgaart. 111-135. & P. Sukabumi-Southern Mountains. p. (2009). Akademie Wetenschappen. A. based on continuous core samples from 1934 BPM well Bodjonegoro 1. Bronto. Proc. Fourth Pacific Science Congress. Petroleum Assoc. (IPA). L. E of Cepu.Geological map of Java. Kon. 47-61. Conv. S.C. Proc. 61-64. Borelis 1 and Alveolina 1. Indon. Mainly shallow marine miliolids. Entire late Early Miocene. stratigraphy) Bothe. and its implications'. Deep water benthic forams from same well described by Boomgaart.pdf) (Distribution of benthic foraminifera in samples from Late Pliocene. Dano and Cibaliung volcanic complex. 419-425. 4th Ann. Indon. Thesis. 6. One of first examples of use of benthic forams for paleobathymetry interpretation. Survey Indonesia. Bogor-Cianjur. Memorie Scienze Geol. menardii zone) planktonic foraminifera. Assoc.. S.Peninjauan kembali Formasi Nglanggran serta implikasinya terhadap mula jadi dan penamaan satuan batuan resmi di Kabupaten Gunungkidul. 89-101. Conf.. Miocene Early and Middle Miocene. Hartono & B. 24 Oligo-Miocene paleo-volcanic centers identified in W part of S Mountains of C Java. Gunung Kidul.3 Ma). p. 6. 1. Mulyaningsih (2008). Four groups: Parangtritis.Batuan longsoran gunungapi Tersier di Pegunungan Selatan. Mulyaningsih (2005). 1. p. Cianjur District. Jakarta06-OT-09.Z. 37th Ann. General stages of volcanic evolution: (1) Oligocene basaltic pillow lavas in Kebo-Butak and Watupatok Fms. Jiwo Hills. Kapubaten Cianjur. used for megalithic site Punden Beruntak) Bronto. Kecamatan Bayat..Identifikasi gunung api purba Pendul di Perbukitan Jiwo. G. (Extended Abstract) (Volcanic arcs of Paleogene. S. Geosc. ('Identification of the ancient Pendul Volcano in the Jiwo Hills. 171-194. Bandung. P. Koswara & K. Southern Mountains volcanism may be continuous from Late Eocene to E Miocene) Bronto. W Java) Bronto. p. Yogyakarta. Proc..vangorselslist. Yogyakarta 2007. (3) destruction of composite volcanoes to form calderas and pumice-rich Semilir Fm. Ages of volcanism at Pendul volcano in Bayat in particular and in S Mountains into four periods: Paleocene. C Java’) Bronto. p. 2012-GD-01. Proc. 269-284. Spec. Geologi Indonesia 1. Kali Putar dan Jentir. Neogene and Quaternary were superimposed. Geol. G. At E flank outcrop of pillow basalt lava flows. S. S.8 ± 6.Geologi Gunung Padang dan sekitarnya. Indon. Hartono & S. and among them intra-arc basins developed) Bronto. Proc. ('Geology of Gunung Padang and surroundings. Hartono & D. S. Yogyakarta. Basal andesite columnar structure. S.. In: Proc. Bijaksana.Potensi sumber daya geologi di daerah cekungan Bandung dan sekitarnya. Putar rivers and Jentir') Bronto. (On energy and minerals potential of the Bandung basin.Bronto. L. J. Assoc. Sanyoto. (‘Genetic relationships between intrusive and extrusive rocks. Workshop Geologi Pegununungan Selatan. Hartono & S. 4p. J. Gunung Pendul is composed of microgabbro (K-Ar age 32. S. Klaten Regency.Stratigrafi gunung api daerah Bandung Selatan. Geol. ('Fossil volcanoes in the Southern Mountains of Central Java'. S. Majalah Geologi Indonesia 19. Hartono (2006). 2. Yogyakarta. Kecamatan Bayat. Bibliography of Indonesia Geology.Hubungan genesa antara batuan beku intrusi dan ekstrusi di Perbukitan Jiwo. Conv. (2009).Pacitan. Publ. Geologi Indonesia 1. (Review of Late Oligocene Nglanggran Fm volcanic breccias and agglomerates of S Mountains. Jakarta 2006 Int. A. C Java'.and extrusives probably remnants of eroded ancient volcano. 44-49. (IAGI). 27th Ann. E. Petroleum Assoc. (2) first construction of andesitic cones of Mandalika and Wuni Fms. Kabupaten Klaten-Jawa Tengah. Volcanic complex. (IPA). E Oligocene andesite age (32. Klaten. (IAGI). Wonogiri-Wediombo and Karangtengah. (2010). Ngkoimani. p. Indon. G.147-163..Fosil gunung api di Pegunungan Selatan Jawa Tengah. Ed.A new perspective of Java Cenozoic volcanic arcs.Jawa Barat. & D. studi kasus di Kali Ngalang. J. Jawa Tengah.6 Ma in Surono 2006).0 19 www. Conv. ('Tertiary volcanic gravity slide rocks in the S Mountains near Yogyakarta. C Java) Bronto. Herman (2012). (Review of Java Paleogene volcanism) Bronto. p. Proc. 1. Majalah Geol. p. Assoc. Budiadi & G. 4p. Kab. Sumber Daya Geologi 20. In. 41st Ann. 38. Indon.com Sept 2016 .. 9-18. Conv. Late Eocene-Early Oligocene. probably deposited on ocean floor. Jawa Barat.Tinjauan volkanisme Paleogene Jawa. G.Sudimoro. and (4) second phase of construction of andesitic cones of E Miocene Nglanggran Fm) Bronto.3 ± 0. special study at Ngalang. & U.Bayat. Lumbanbatu (2006).O. 3. Purwanto (1998). Bayat. 3-13. S. West Java'. Pusat Survei Geologi.. S. 195-204. Hartono (2006). (IAGI). S. Indon. p. Indonesia 20. Bandung. Astuti (2004). Geol. Baturagung. South Bandung mountaineous area. Indriana & M.S. (Geological overview map and explanation from E Java to Sumbawa. schaal 1:1 000 000. not N5 as suggested?. high plain of Pangalengan and Bandung city eleven Pliocene. p. (Extended Abstract) (Sediment thickness below Kendeng-Rembang zones 11. S. Hartono & B. 2-16. 131. HvG)) Brontodihardjo. 788-806. (Late Oligocene Kebo-Butak Fm at Baturagung escarpment. Res. (IAGI). S. p. Lombok. Jakarta 2006 Int. composed of volcanic sandstones and calcareous sediments.0 20 www.Yogyakarta. Geol. deposited in submarine fan environment. Jiwo. G. Jaarboek Mijnwezen Nederlandsch Oost-Indie 44 (1915). Bibliography of Indonesia Geology. Centre (GRDC). Bataafse Int. C Java) Brotopuspito.. Proc. Purwanto(2002). 2. 79-92. Report EP-37680. Interbedded deep marine limestone with planktonic foraminifera. Madoera.000.Waduk Parangjoho dan Songputri: alternatif sumber erupsi Formasi Semilir di daerah Eromoko. Central Java). 5p. (On Juwangi calcarenitic limestones near Kedung Ombo. Dev. J. sheet 17 of 1:1 million map series. Mulyaningsih. (Oligocene? pillow basalt lava flows exposed at Opak River. Verhandelingen 2. Bayat area (Klaten.Stratigraphy of the younger Tertiary in North-East Java and Madura. Geol. Petroleum Maatschappij (BPM). Bali. Conv. (Two alternative eruption centers for pumice-rich acid volcanics of E Miocene Semilir Fm in the Eromoko area. (Unpublished) Budhitrisna. Small hill ~15 m high and 150 m away from river to W was eruption source. S Mountains. (1987). Petroleum Assoc.Geologic map of Tasikmalaya Quadrangle. S of Wonogiri. Central Java. Ed. S. latest Oligocene. H. Geosciences Conf. 3-54. 117-128. 1-41. Sandstone composed of very angular volcanic glass grains. Pambudi & G. Assoc. 161-188. (IAGI). incl. 3. Mulyaningsih. Assoc. T. S. Surabaya.Geologic map of Salatiga Quadrangle. Geologi Sumberdaya Mineral 12. Hartono (2002). Lavas overlain by pumice-rich Semilir Fm volcaniclastic rock (Early Miocene).Rembang zone. p.Batugamping kalkarenit Juwangi dan masalah penggunaannya sebagai Batu Bahan Urugan bendungan Kedung Ombo di Jawa Tengah. Hartono & D.Quaternary rock units (nine volcanic) over subsurface Miocene volcanic rocks) Bronto. K. Geologi Indonesia 4. p. (1915). J.A. W of Watuadeg Village.. Astuti (2008). (1984). with Kendeng deeper than Rembang) Brouwer. Proc. J. 6. probably unconformable over basaltic pillow lavas) Bronto. SE Java) Bronto. All islands on this map Neogene sediments and young volcanics only) Brouwer. Globorotalia kugleri (= lower N4. Bayat area (Klaten.. West Java'. Toelichting bij Blad XVII (Oost Java. 13th Ann. 1408-6.P. (1957). 31st Ann. Soembawa).Sedimentary rock thickness at Kendeng.13. Indon..D. Nukman (2006). Centre (GRDC). Bandung. >650m thick. Hartono & B.('Volcanic stratigraphy of the South Bandung region.000.Gunung Api purba Watuadeg: sumber erupsi dan posisi stratigrafi. Budhitrisna. R. Sleman. Kabupaten Wonogiri.Indonesia. Indon. T. S Mountains. and hyaloclastites. Bandung. as constructed based on regional Bouguer gravity anomaly map.. p. Indon. The Hague. scale 1:100. Astuti (2009). A. (1992). J.com Sept 2016 . (Same as paper below) Bronto.vangorselslist. Geol. probably products of nearby submarine volcano. (IPA). p. Associated with pillow basalts. S. and Exhib.The genesis of volcanic sandstones associated with basaltic pillow lavas: a case study at the Djiwo Hills. scale 1:100. Pambudi. Proc.The genesis of volcanic sandstones associated with basaltic pillow lavas: a case study at the Jiwo Hills. Res. S. OT-44.P.000m. S. Globigerina tripartita. Central Java). Geologi Indonesia 3.Geologische overzichtskaart van den Nederlandsch-Indische Archipel. Conv. Jawa Tengah. G. G. Dev.000. p.. S. Geol. G. binaiensis. Lunt & T. Geol. 1995. Geol. Budiman. possibly Eocene sandstones. generally N of most E Java fieldtrips. B.technical analyses. Res. p. 305-309.IPA Fieldtrip to Eastern Java. Geol.E. Ser. Silalahi (1994). 330-335. Foraminifera studied by Saint-Marc & Suminta. Proc. Explanatory notes and map. S. Prakarsa (2000). (IAGI). (IAGI). (Semarang-Surabaya route. Bandung.Konsep ekplorasi hidrokarbon untuk Formasi Parigi di Cekungan Jawa Barat Utara. Ed. C Java. Indon. p. Conv. p. 2002. Centre (GRDC). especially in lower part of section) Burgon. G. Java. a dividing line between Tertiary structural patterns in Sumatra and Java islands. 2012-EG50. M Miocene limestone play) Budiyani. Priambodo & B. etc. Geologi Indonesia 3.. (E Java Basin M Miocene Ngrayong Fm sandstone in Gondang area in submarine fan facies. I. Budiman.Pliocene Njepung section.. Allan (2002). Budiyani. Dev. Res.0 21 www. p. 180-198. documenting Early Miocene? uplift event. (IAGI).E Pliocene Thalassiosira convexa zone. & Y. 6.Budiarto R. (1976). Pringgoprawiro et al. with some chemical.a structure. 11-20.Komplek mud volcano Kradenan. 140-154. D. Lower part of Globigerina marls in Late Miocene. (Marine diatoms from Late Miocene. Mudi.The causative body of the old Ungaran volcano based on a gravity data model.Penyebaran Formasi Ngrayong sebagai penghasil hidrokarbon di daerah Gondang dan sekitarnya cekungan Jawa Timur. Geol. 9-15. M. (2012). S. Geoph. Willumsen (1995). p.com Sept 2016 . p. & P. Indonesian Petroleum Association. Burhannudinnur. Assoc. See also Mannhardt 1920. Yogyakarta. J. (3-day trip to Sekarkorong. Conv.1979. Gravity high interpreted as basement high. (1922).Geology of the Besuki Quadrangle. 41st Ann.Remodeling geology of Parigi reservoir at Tugu Barat. Bouwk. (Interpretation of N-S gravity profile of Karangsambung area. Ind. 363-368. No ties to surface geology) Budisantoso Pendowo (1991). 29th Ann. G. Proc. Wikan Haksara (1991). p. Field trip Guide Book. With log crosssections and examples of seismic mounding) Buning. Proc. 1. Indon. middle part M Pliocene Nitzschia jousea zone. 1-6. F. Conv. Java. Assoc.Sunda Strait. with stops at Kali Lutut. Open oceanic environment with strong upwelling suggested by presence of Thalassiosira nitzschioides. 1977) Burckle. Dev.Het voorkomen en de ontginningswijze van natuurasphalt in verband met de asphaltexploitatie te Cheribon. (On the occurrence and exploitaton of natural asphalt near Cirebon. p. (2000). Marine Micropaleontology 7. North West Java Basin. Assoc. Probably fed from overpressured Early Miocene Tawun Fm) Bibliography of Indonesia Geology. 23rd Ann. (1996). Kendeng zone. Tijdschrift 25. Conv.Indonesian Petroleum Association East Java Fieldtrip October 13-15. Mukmen & L. I. Indon. Kalipanjang) Burgon. Proc.H. Geol. (1982). ('The Kradenan mud volcano complex'. 1. ('Hydrocarbon exploration concepts for the Parigi Fm in the NW Java Basin'. p. Centre (GRDC). Bromo. p.Diatom biostratigraphy of Late Miocene and Pliocene sediments of eastern Java (Indonesia). Bandung. Geol. Sumberdaya Mineral 6.e) Burhanudin. L.Main fault structure of Karangsambung area based on gravity model. (IAGI). 20th Ann. E Java. Indon. 60. IPA Field trip Guide Book. p. P. 141-150. & A. Geol. 33 p. Ngepon. 1-68.vangorselslist. Jakarta. Assoc. Indon. (2014). A.The Cibaliung gold deposit. Paleocurrent directions from flute casts suggest main sediment supply from NW (opposite of presumed southern origin of volcanic provenance in Ngawi area?. Mud probably sourced from Tawun Fm) Cahyo. Review of mud volcanoes. Conf. 2004. HvG)) Bibliography of Indonesia Geology. hosted in Neogene volcanics. dry condensate gas. 2007) Carnell. p. NE Java basin. narrow pinnacles to broad platform deposits. IPA07-G-116. Miocene-age mineralization (~10 Ma).iagi. 35th Ann.. (Outcrop study of Late Miocene Kerek Fm calcareous sandstone turbidites in measured sections in Kedungjati area. MINDAGI (Trisakti University) 7. 300-304.B.. These carbonates have different morphology. M. IPA11-SG-036. (eds. 19-25. A. I. I.The Rajamandala limestone of the Sukabumi area of West Java. Malda. 561-567. (IAGI). Other areas of Cepu platform drowned in Oligocene. petroleum gas. A13-A14. In: S. Noeradi. (IPA). (Carbonate build-up morphologies in Cepu Block vary from steep-sided. Indon. Geol. 18 p. I. Central Java: an analog for sandy Miocene Formation in western Kendeng Zone. Prihatmoko (2005).L.vangorselslist. J. Petroleum Assoc.C. can it be considered a field analogue for the Baturaja limestone. (AAPG) Int. Assoc. Jakarta. Buildups developed on isolated platform that began to form in E Oligocene.. Abdassah (2012).A. Burgess (2007). D. A. 41st Ann. Thicker buildups drown in E Miocene and are covered by M Miocene clastics that are low quality seals. Proc. with morphologies related to underlying extensional faults and subsidence rates across platform. Berita Sedimentologi 26.variations in Oligo-Miocene carbonate buildup morphology. Buildups up to 2 km thick. F. (Late Oligocene Rajamandala reefal limestone of W Java outcrops between Cibadak in W and Bandung in E. Geol. surrounded by foraminiferal/algal dominated shelf sediments. p. 6. Field Trip Guide Book. (IAGI) Spec. Jakarta.Burhannudinnur. First discovered in 1992.Pergerakan sedimen bawah permukaan (PSBP) di Jawa Timur. Issue. creating small pul-apart basin (see also Harijoko et al. 2012-EG49. Bali. M. Conv.or. Fardiansyah & C. O. Indon. Conv. (IPA). Carnell. (Cibaliung low sulphidation epithermal Au-Ag deposit at SW tip of Java. Depositional environment interpreted as lower submarine fan system.id/fosi/files/2013/05/BS26-Java. Assoc. etc. Fardiansyah.A.) Burhannudinnur. Ed. (online at: www. Proc. p. SPE Indonesia Branch. drowning at different times. HvG)) Cahyo. Rajamandala Fm often regarded as analogue for oil-productive Batu Raja Lst of S Sumatra and NW Java. formed at shallow depths (250-300m). Conv. F. Proc.com Sept 2016 . 1. W Kendeng zone. Petroleum Assoc. Western Kendeng Zone (North East Java Basin).F. decision to mine in 2004. Deposition interpreted as series of small coral islands. resulting in isolated carbonate buildups. American Assoc. but they are not direct age equivalents (Batu Raja Fm age is of Early Miocene age. Yogyakarta.Karakter mud volcano di Jawa Timur.. 45-57. carbonate deposition ceased over parts of platform while other areas continued to grow. Petrol. 9-34.pdf) (similar to paper above) Cahyono. Price & S. (2000). Prasetyadi (2011). B. Through Late OligoceneE Miocene. Jakarta. Site possibly influenced by NW-SE Sumatra Fault system. p. ('Character of mud volcanoes in East Java'. Banten: discovery to decision to mine. Prihatmoko et al. 46p. 31st Ann. Proc.3D modeling of Kerek turbidite sand bodies based on outcrop study in Kedungjati area.Three-dimensional facies modeling of deepwater fan sandbodies: outcrop analog study from the Miocene Kerek Formation.The Rajamandala limestone at Sukabumi. p. lower reservoir quality and more clay-rich seals and commonly contain large gas columns) Carlile. Mud volcanoes of Randublatung zone. Malda & C. O. ('Subsurface sediment movement (PSBP) in East Java'.) Indonesian mineral and coal discoveries.Cepu 3D seismic. Prasetyadi (2013). Geol. p. & C. contain variety of gases: biogenic gas.0 22 www. Sapiie & D.. Indon. (1996). Leipzig. Banten Block. 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Descriptions of 26 Lepidocyclina species from Oligo-Miocene samples from C and W Java and Madura. Indon. C. N. zone 12 warm zones. (1932). Conv. 1896 (Abstract). ('Lepidocyclinids from Java'. 171-204.B. Dyer. Geol.L. PACRIM 2015 Congress.5 Ma.U. Chan. Zone 9 (transitional. Klitik Fm: zone 11 cold.S. Seismic Atlas 2. Selenka & M.0 23 www.Y. 3. Kluwih. Zone 4 warm (NN14-NN15). (HAGI)-Indon. A. S. 12a. In: Proc. S.cold zones. AAPG Foundation Grants-in-Aid Recipients 1999.L. NN19 and NN20. 80-94. Ngawi. ('On the geology of Java. 83. A. Melbourne. Zone 6 (warm.J. NN15). Engelmann. Kalibeng Fm: transitional zone 3 (NN13-NN14). Geol.. many species names probably synonyms. Zone 7 (cold zone. (1939). Berita Sedimentologi 29.M. B. insbesondere des Ausgrabungsgebietes. 4p. Australasian Inst. HvG)) Caughey. Indon. C. (IAGI). p. Kerek Fm Zone 1 and 2 warm zone and cold zone of lower NN12 and NN12-NN13 respectively.Zur Geologie von Java.. Medan. p.. Indonesia. Eastern Java. 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(2015). and Irian Jaya.alteration and implications for potential porphyry Cu mineralisation. JCM2013-0005. Assoc.Paleoclimatic interpretation using calcareous nannoplankton. Petroleum Assoc.A. Verhandelingen Geologisch-Mijnbouwkundig Genootschap Nederland Kol. (1999). SW Java. No location info) Chandra. Banten Province. Natuna.iagi. NN16). and Zone 10 (warm. 35-46. Zone 8 (warm. J. NN16).or.b. ('The foraminiferal fauna from some Cycloclypeus-bearing rocks of Java'. & R. Indon. Haryono et al. Indonesia. Ed. (Late Miocene to M Pleistocene of Kendeng zone shows climate changes in nannoplankton. Priangan and Purwakarta. (Cu-Ag-Au mineralisation at Kluwih prospect in E Java. Ser. Indonesia related to high-sulfidation hydrothermal system within dacitic volcanic dome.U. Kalimantan.B. Geol. Assoc. SW Java. C. Miocene larger forams from Java localities S Kediri. Rahardjo & Dardji Noeradi (2013). 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Hall (2007).0 24 www. Soc. Somm. West Jiwo Bayat. 6. B. Pekanbaru. Geologique France. Left-lateral strike slip faults at N70° offset Quaternary intra-arc and volcanic chain) Chotin. S. Assoc. 47-59. Bull. and Exhib. N135° and N165°. Ph. Jakarta. 4. J. Bull. Triwibowo (2002). 5. Indonesia. R.Pliocene in Solo River. L. P. N70E strike-slip fault is reactivation of pre-Neogene Sundaland margin) Clements. Much of quartz is from lowgrade metamorphics) Clements. Giret. Geosciences Conf.U. J. (IAGI).Gamping daerah Sekarbolo. Jawa Tengah. 175-177. A. Hall (2006). Petroleum Assoc. S. p. L. ('The sedimentation associated with a major strike-slip fault in the central part of the island of Java. New structural model for W Java suggests major thrusting in S Java has previously been overlooked. Suminta & N. Indon. Bandung.com Sept 2016 . Java fault systems determine locations of volcanoes along N 000 and N 045 tension gashes. Thesis Royal Holloway. University of London.vangorselslist. N70°. Proc. Another arc jump since Late Miocene and modern Sunda Arc volcanoes now on deformed Late Miocene arc products. Geologique France 26.Interpretasi paleotemperatur berdasarkan nannoplankton lintasan S. Geol.P. B. Arc became emergent during Late Oligocene.Choiriah. C Java') Choiriah. p. N 070 strike slip zone marks boundary between western subduction system and eastern collision-subduction Australian system) Chotin. (IPA). Bibliography of Indonesia Geology. & R. Ngawi. un enregistreur des mouvements tectoniques a l’aplomb d’une zone de subduction. In C Java eeper structural level is exposed and arcs have been removed by erosion. Jiwo Barat Bayat. C Java') Chotin. & R.J. Hasjim (1984). Java fault systems N30°. rarely did its products reach Java. P. B. Indonesia'.Paleogene to Early Miocene tectonic and stratigraphic evolution of West Java. Klaten. N90°. IPA07-G-037. Klaten. from North.D. Assoc. Kurniawan & Surono (2006). Conv.Gamping limestones in the Sekarbolo area. 29th Ann. Ed. 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Late Miocene resumption of volcanism N of Paleogene arc. Proc. S..Foraminifera besar pada satuan batugamping formasi Wungkal.E. ('Nannoplankton biozonation of the Wungkal Fm in the Gunung Pendul area. a record of tectonic movements up a subduction zone’. Indonesia. (2008). (IPA). J. 6. Geol. Ritha. D. Vienna.Oligocene quartzose formations sourced from Sundaland. Mid-Cretaceous zircons in U Eocene. W. 1. and W Sulawesi arc developed later. C Java displays deepest structural levels of N-directed thrusts. Geol. with wide zircon age ranges (Proterozoic.L. M. Paper 487. Jakarta.E Paleogene local volcanic arc source. L.W. Geophysical ReseEGU General Assembly 2010. p.Detrital zircon U-Pb age and Hf-isotope perspective on sediment provenance and tectonic models in SE Asia. 145-74 Ma (Cretaceous). online at: http://meetingorganizer.vangorselslist. (IPA). (Abstract only. K. Late Eocene Bayah Fm higher contribution of E-M Cretaceous granites from Borneo Schwaner Mts) Clements. overthrust arc largely removed by erosion. Hall. America (GSA). Late Cretaceous and Paleogene zircons derived from two volcanic arcs in Java and W Sulawesi. Smyth & M. R. B. IPA08-G-115. and active cross-arc extensional faults. Permian-Triassic zircons from granites in SE Asian Tin Belt. N Serayu Mts folds and at S border Cretaceous ophiolitic basement and melange outcrops of Lok Ulo) Cook. Ed. Kangean PSC.Eocene).pdf) (Java island complex history of volcanism and unusual subduction characteristics. 1-17. extension related to development of Makassar Straits. M Eocene. Belousova.U-Pb dating of detrital zircons from West Java show complex Sundaland provenance. E. Proc. Griffin & N. Petroleum Assoc.Y. Pardyanto &. and derived from Malay Peninsula and Tin Islands granites. (Ages of zircons from M Eocene volcanoclastic Ciletuh Fm indicate Late Cretaceous.. Development of 1 TCF GIIP complicated by shallow gas in overburden and faults. some with seabed expression. Dev. with potential mass flow features. In: E. (U-Pb age populations of zircons in Paleogene formations in W Java: 80-50 Ma (Late Cretaceous-Paleogene). D. L. In E Java volcanic arc thrust onto thick volcanic/sedimentary sequence formed N of arc in basin due largely to volcanic arc loading) Clements. W Java arc now thrust onto shelf sequences that formed on Sundaland continental margin. Petroleum Geoscience 15. B. Zwaan (2003). (Terang-Sirasun reservoir Plio-Pleistocene Paciran Fm Globigerina calcarenites. Episode of Late Miocene thrusting at ~7 Ma observed throughout Java linked to Nward movement of volcanic arc. p. Java arc was active before microcontinent collision.. S.org/EGU2010/EGU2010-12437. R. 1996) (Map of C Java Dieng Plateau.0 25 www. Little geology info) Cottam. Cottam (2009).Lw Oligocene derived from granites of Schwaner Mts of SW Borneo. H. 19p.J. 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Presence of glaucophane suggests High P metamorphic 'accretionary' basement. M. from Ngampel. S of Surabaya (= just N of Lusi/ Sidordjo mud blowout. (Distinctive cidaroid echinoid spines from M Miocene Bulu Fm.Djuri. Alcheringa 34. Selenka & M. (1973). Geol. ('Notes on the stratigraphy of the sediments in the Trinil region'. (Extended Abstract) (E Java Basin three main intervals of carbonate platform and mound growth: Kujung (carbonate mound and off-mound. Petroleum Assoc.Les foraminiferes des couches de Rembang.000. Simo. (1975). omphalus. De Mijningenieur 11. Reichs-Museums Leiden. D. Naranjo & A. Tang.Quelques foraminiferes de Java.M. W...repository. p. Renema & D. HvG) Bibliography of Indonesia Geology. Miocene Cycloclypeus annulatus and Lepidocyclina papulifera n. Java.. Carroll (2006). 5 km NNW of Sale. H. N. and Wonocolo (Bulu limestone. Material from extinct mud volcano of Pulungan. 279-294. 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Assoc.Preliminary notes on the age of Miocene limestones from South East Java to Sumbawa. Gaffar (2014).ll. (IPA). Hattori. Marine Petroleum Geol. Indon.pdf) (Gravity and magnetotelluric modeling around WSW-ENE trending Cimandiri Fault Zone. study for paleomagnetic reconstruction of the W Java area') Bibliography of Indonesia Geology. 97. Indonesia. P.. Febriani. p.M. Yoshino. p. which runs between Bandung and Pelabuhan Ratu. Gunung Kidul. 311-365. Nurdiyanto. With some remarks on Tertiary stratigraphy) Flathe. p.E Pleistocene) Fermin. M. Galena & C. Thesis Chiba University. 2. Robba & D. Prasetyadi (2013). Widarto. Yogyakarta. E. Effendi. East Java. Palaeontographica 60. 2012-SS-04.com Sept 2016 . investigated by SAR interferometry.Control of syn-contractional sedimentation of Kendeng fold thrust belt: new perspective analogue to evaluate risk associated with trap formation. (Age of Wonosari Lst in eastern Southern Mountains of SE Java with Flosculinella bontangensis (Lower Tf larger foram stage= planktonic foram zone N8-N9 or slightly younger)) Fukushima. L. N. 1-154. R. p.jp/metadb/up/thesis/SGA_0071. Mori. Petroleum Assoc. Yogyakarta: an explanation the dynamic process from Upper Sambipitu Formation. (IAGI)..Die fossilen Anthozoa aus der Umgegend von Trinil. West Java. 629-638. 27th Ann.Audio frequency magnetotelluric imaging of the Cimandiri Faullt. 5p.. Kano (2009). W Java at end-Mesozoic. (Volcaniclastic turbidites of E Miocene Sambipitu Fm are distal turbidite facies on slope to basin floor. Felix. Terrain here called sinus karst because of sinusoidal contour of rounded hills which rise 30-70 m above floor.N. Jakarta.A. 41st Ann. (online at: http://mitizane. p. Indonesian J. A.0 34 www. J. Anom. Purnamasari. Java’. J. Geol.C. 6.Grundzuge der Morphologie. Y. 1-11. 1. A. & N.The stratigraphical distribution of the larger foraminifera in the Tertiary of Java. Geologi Sumberdaya Mineral 10. Gerth. With one plate) Gerth. Martin. Martin. (1929). Sammlungen Geol.Geological map of Java and Madura. p. 2. CCOP Techn.M. Geological Survey of Indonesia (1963/1977).Penampang geologi sepanjang Jawa Tengah. Verbeek.Genesis of cockade breccias in the tectonic evolution of the Cirotan epithermal gold system. Good example of mineralized cockade breccia. R. S. Verbeek und von anderen bearbeitet durch Dr. K-Ar age of adularia of Cirotan vein 1. Dev. (Pliocene Cirotan gold deposit up to 25m thick and hosted by Pliocene microdiorite (4. Amsterdam. etc. Schiller. Siemers & J. Geol. 497-520. K. Syaifudden.T. p.Echinoidea. R. Milesi (1996). Petroleum Assoc. (IPA). E.A. van Gorsel (1990). 387-445. Martin. Bull.) 1.Gafoer.com Sept 2016 . Reichs-Museums Leiden (N. in right-lateral strike-slip fault that evolved to normal fault at end of development. Bandung. 392-395. H. Marcoux & J. 7-12.Geological map of Java and Madura. 111. (1930).knaw. (online at: www. Rutten and others.. 86 p.000.Miocene outcrops of Cibadak. (1921).M. Bayah. p..) 1. Nederl. Kon. With 3 plates) Gerth. Canadian J. In: Die Fossilien von Java auf Grund einer Sammlung von Dr. Ratman (1998).vangorselslist. Martin's 'Fossils of Java' series.Ein neues Eocaen-Vorkommen bei Djokja auf Java. Ganie. Sheet II.P. Akademie Wetenschappen.D. A. Ed.F. self-organizing system in fault zone) Geological Survey of Indonesia (1963/1977). S.. H. (online at: www. West Java. 4. Rajamandal Limestone W of Bandung with only Coeloria singularis Martin (= only Late Oligocene corals known from Java?) Typical Pacific assemblages. Proc. Breccia formation of hydrothermal origin.1 Ma. p.M. (4-day fieldtrip to Eocene. J. 33. scale 1:500. Centre (GRDC). 17-32.0 35 www. in active. Reichs-Museums Leiden (N. Martin. K. 19.naturalis. (Short paper with larger foram distribution table. Sammlungen Geol.Echinodermata. Geological Survey of Indonesia (1963/1977). 591-599. In: Die Fossilien von Java auf Grund einer Sammlung von Dr.repository. A. Proc. p.000. ('Geological cross section from Central Java to West Kalimantan') Gafoer. Garrard. with descriptions of ~42 species of EocenePliocene echinoids from Java collections of Junghuhn. p.Geomorphological features in the Eastern Sunda Trench. Bandung. B. M.D. IIB.pdf) Bibliography of Indonesia Geology.IPA Post-Convention fieldtrip. (online at: www..Geological map of Java and Madura. (2000).SouthWest Java.000. H. 6. Jebrak. C. Earth Sci. West Java. 2nd ed. Superman & E.naturalis.repository.5 Ma). Ciletuh and Pelabuhan Ratu areas) Genna. East Java. Bandung.nl/document/552457) (Part of K. 4 th Pacific Science Congress.Kalimantan Barat.Geological map of western part of Java. Indon. 33. not much new) Gerth. Res. Bandung.dwc.nl/document/552456) (Tertiary echinoids chapter in K. R. Eocene (Nanggulan) and MiocenePliocene corals from collections of Verbeek.F. Sheet I. Verbeek und von anderen bearbeitet durch Dr. 2. H.000. Martin (1891 and later) series on Tertiary fossils of Java. scale 1:500. Sheet III.nl/DL/publications/PU00015901.7±0.5 Ma) that cuts Miocene volcano-sedimentary series with rhyolitic ignimbrite (9.T.Coelenterata-Anthozoa. 93-102. scale 1:500. Honza (1987). Central Java. 1:500.M. p. D. (1922). 3. (‘A new Eocene locality near Yogyakarta on Java’. Gertisser. Unconformities between Pretertiary and Paleogene and between Paleogene and Neogene reflect Tertiary orogenic phases: main phase at end of Neogene. S. 196. Composed mainly of fresh-water diatoms Cymbella.000 years BP and ~31. p. Excursion D1. P.000 years BP in S part of basin. Palaont. Rundschau 22. (1854).e. The Hague.R. p.Neue Beitrage zur Kenntnis der Korallenfauna des Tertiars von Java. (1931). Plains of Darma. C. Illustrated in Junghuhn (1850) and thought to be of Miocene age by Verbeek and Fennema (1896) and Martin (1914). Oppenoorth (1929). H. Little stratigraphy and locality information) Gerth. p. Fort. Mieling. 60m) zones P15-P19 (Late Eocene-Early Oligocene)) Grandjean. Java 1929. I. With cross-sections. 3. ('On the Tertiary flora of Java') Grandesso. Fourth Pacific Science Congress. Reinhold (1933). Borobudur temple was never buried under volcanic material during historic times) Goppert. nach den Entdeckungen des Herrn Fr. Padova.W. 1-7. Die Korallen des Eocaen und des alteren Neogen. (online at: http://books. ('The geologic framework of Java'.com/books/ ) ('The Tertiary flora of the island of Java. M.R. White limestone outcrops of Gunung Gamping. i. collected by Junghuhn.Borobudur. 3. Nitzschia and Gomphonema. Typical reefal limestone with common coral. 245-264. stratigraphic columns and tables) Gerth. 3-4. R. H. Several generations of paleolakes in Borobudur basin and Borobudur Temple probably stood by water body. a basin under volcanic influence: 361.Die Tertiarflora der Insel Java. Volcanic activity strongly influenced evolution of basin.F.000 years BP to present. F. (Borobudur basin N of Yogyakarta City. H. Volcanology Geothermal Res. J.. ('The diatomaceous earth of Darma in Cirebon'. different facies from nearby Nummulites limestone localities of Jiwo and Nanggulan) Gerth. Bibliography of Indonesia Geology. 177186. described and placed in context of total flora of the Tertiary period'. C. 1864. De Mijningenieur 14. (1864).The Upper Eocene Nanggoelan beds.google. and species from Oligo-Miocene of Rajamandala. Murwanto (2010). 40-46. p. Lahitte. J. surrounded by three andesitic volcanoes: Merapi. & W. Ed. Geol. (1933). Wassmer.vangorselslist. Neues Jahrbuch Mineral. Serayu and Rembang areas. & T. 6. Degroot & H. S. M. Only three areas of Pretertiary outcrop. SW of Kuningan. Navicula. Wetenschappelijke Mededeelingen 25. S of Darma. Today’s active volcanoes appeared in Quaternary. Hadmoko. 188-200. Two major volcanic deposition events up to tens of meters thick at ~119.com Sept 2016 . 200m) with planktonic foram assemblages of zones P11. P. p.0 36 www. Dienst Mijnbouw Nederlandsch-Indie. (2001). Descriptions of four species of solitary corals from Nanggulan. 53.F. 23-28. 4 km W of Yogyakarta. p. below thick cover of Tertiary sediments. Lavigne. H.B. P.De diatomeeenaarde van Darma in Cheribon. Junghuhn beschrieben und erortert in ihrem Verhaltnisse zur Gesammtflora der Tertiarperiode. S of Ciremai volcano.Uber die Tertiarflora von Java.P14 (M Eocene). p. The corals of the Eocene and older Neogene'.R. Gomez. I. but abundant Pellatispira and some Nummulites demonstrate Late Eocene age. Junghuhn.. p. Merbabu and Sumbing. Charbonnier. H. Synedra. ('New contributions to the knowledge of the coral fauna of the Tertiary of Java. V. lake deposits with interbedded fine Ciremai tuffs and ~15-40cm thick beds of white diatom earth. (Nanggulan section W of Yogya: lower part (Kalisonggo Mb. Geol. First description of Tertiary plant leaves and petrified wood fragments from Java.Contribution to biostratigraphy of the Nanggulan Formation (Java) based on planktonic foraminifera. Melosira. upper part (Seputih Mb. Janin. W of Yogyakarta.Der geologische Bau Javas. 1-169. 1-45. Memorie Scienze Geol. after discoveries of Mr Fr. Mainly from 3 localities) Goppert. 287-295.CP 16 (M. S. J.) (First paper on calcareous nannofossils of ~70m thick section of Wungkal Fm.dwc. p. AAPG/ IPA Int. & E.B. Jakarta.go.Potensi hidrokarbon di sub-cekungan Banyumas. Akademie Wetenschappen. A. (Calcareous nannoplankton zonation of Nanggulan Fm. Proc. S. Jawa Tengah bagian selatan.jp/. 20km E of Yogyakarta. Johnstone. 8. 1096-1104. Geol. on the South coast of Java. M.J. JCM2011-474. Indon.. Makassar. Spiker (1932). J. Japan (Chishitsugaku Zasshi) 106. Haanstra. 5. (online at: www. Fauzan (2015).. (1889). Asch (2014).jst. Geosc. Jurnal Teknologi Mineral (ITB) 8. Discoaster barbadiensis and Cribrocentrum Bibliography of Indonesia Geology. Stevens & D.5E). Proc. R. Jakarta 2006. U. Central JavaIndonesia. 36th HAGI and 40th IAGI Ann. Setyoko (2011). marls and quartz sandstones. Widodo (1982). (IPA). Ed. N Java’. H. Images show asymmetrical crustal structure and can be interpreted to show low-velocity continental fragment or remnant of Woyla Arc in south coastal area (E of 110°E). Syaiful.P. Scottish Geogr. 4.G. which has been accreted to Sundaland margin. Amsterdam 35. ('Hydrocarbon potential of Banyumas sub-basin. Banyumas Sub-basin numerous oil and gas seeps. 2. Ruswandi & Y.Early Oligocene/CP 16c. Oil from seeps of fluvio-deltaic kerogen origin) Guppy. A. of which 17% Recent) Haberland. Bayat area. p.P. Indon.Calcareous nannoplankton biostratigraphy of the Nanggulan Formation. 20p. Drevet. 10. Soc. p. Sapiie. A. Eocene-Oligocene boundary recognized by last occurrence of Discoaster saipanensis. Molluscs 47 species. 5 p.Karren carbonate rocks. likely reflecting ophiolitic. J. Used in Java sugar industry for filtration raw cane sugar solutions and insulation of pipes) Gross. A.age probably Pliocene. B. T. J. Range from Late Eocene/CP 14. Bohm & G.Paleostress analysis of Grindulu Fault in Pacitan and surrounding area its implication to regional tectonic of East Java. zones CP 13. p. p. Source rock identified includes Paleogene of Nanggulan and Late Miocene of Halang Formations.Uber Fossilien aus dem Altmiozan von Rembang (Nord Java).Calcareous nannoplankton of Paleogene sediment from the Bayat area.com Sept 2016 .. (Extended abstract of ExxonMobil NE Java basin study) Gultaf.C. With plate reconstructions of Sundaland region. O.5-111. Proc. Grey and brown-grey clays interbedded with Lepidocyclina limestones. E. L. but unsuccessful.knaw.journalarchive. Sulaeman. E side of Gunung Pendul.. Johnstone (2006)A new look at the East Java Basin using a genetic basin analysis approach. (Seismic travel time data confirms accretionary nature of crust in C Java segment of Sunda subduction zone (109. 96. Petroleum Assoc.Preliminary note on the geological structure of the Sindang-barang district. Bachtiar & A.0 37 www. M. Kon. (online at: www. 39th Ann.East Java Microplate since Cretaceous (80 Ma)) Guntur. C Java. arc rocks and metamorphic rocks of Meratus assemblage subduction melange) Hadi.Field trip guide book Prupuh. J. IPA15-G-059..vangorselslist.. McPherson.. Joint ASCOPE/ CCOP workshop on hydrocarbon occurrence in carbonate formation.Recent paleostress history along SW-NE trending Grindulu Fault in Pacitan District in Southern Mountains of E Java. Asian Earth Sci. Central part of Java crust lower than average crustal velocities. Petroleum Assoc.L Eocene)) Hadiwisastra. H. 651-658. 6. (Descriptions of Early Miocene Prupuh and late Miocene Karren limestone formations for 1-day fieldtrip) Hadiwisastra. Samuel & H. S part of C Java'. (IPA). Kumai (2000). Nederl. Proc. Central Java. Study of molluscs collected by Erb from Ngrayong Beds at N side Lodan saddle. Conv. C.Accretionary nature of the crust of Central and East Java (Indonesia) revealed by local earthquake travel-time tomography. & H.. (2001). 34p. Conv. Sriwijaya. 73-76.pdf) (‘On fossils from the Early Miocene of Rembang.nl/DL/publications/PU00016326.M. Conf. (Analysis of Cretaceous. 9 p. Surabaya 1982.. Several wells drilled. Inter-University Seminar House of Kansai. also malachite. (IPA). B. K.1-6. IPA07-G-035. Conv.P. which is carbonate-cemented and brittle) Hakiki. Subzone CP 16c in upper part of section identified by co-occurrence of Reticulofenestra umbilicus. IGCP-355. Associated rocks are basalt. 137-144. Conv. Cottam (2007). 1-13. p.. Geosc. upper part (Totogan Fm) Oligocene age) Hadiwisastra.osaka-cu.media. Hadiwisastra. and also in basal 50' of clastic section above top carbonate.Depositional setting and distribution of carbonate facies of Wonosari Formation. Sapardina (2015). F. R.reticulatum. Jakarta. 37th Ann. W Java'. (Losses of drilling mud while drilling Oligo-Miocene carbonates in Banyu Urip Field mostly in tight rock of drowning cap of carbonate reservoir.H. Excellent pressure connectivity throughout reservoir from carbonate reservoir to overlying clastic section. Musgrove. East Java. onshore East Java. Sulistijo (2013). F.Biostratigraphy of calcareous nannofossils in the Paleogene chaotic sediments in the Karangsambung area.vangorselslist.P. J. thought to be horizontal fault zone) Hadiyat. (IPA). with low porosity rim of ~8-9% (a gradual diagenetic transition caused by less fresh-water dissolution) Hakiki. Varnai. Early diagenesis associated with exposure to fresh water at sequence boundaries creates cementation and dissolution over 50m cycle. Jakarta.Oligo-Miocene carbonate reservoir quality controls. Indon. p. 1-17. E. Sci. Thesis Institute Teknologi Bandung (ITB). 39th Ann. Not much detail) Hall. Siregar. S. Symp. galena and sphalerite. Hakiki. 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L. Also shoreline displacement of Java Sea toward E since Late Pliocene) Kapid. Bayah and adjacent offshore areas. Uneputty & S. Indon.A. 1. Conv. & S. (Unpublished) Keetley. 26. Buletin Geologi (ITB). Jakarta.l. Kartawa. 6th Ann. (Quantitative analysis of calcareous nannofossils from Solo River. Ledok Fm roughly NN11lower NN12/ D. Ed.A.Batas umur Pliosen/Plistosen berdasarkan analisis nanofosil pada lintasan sungai Bengawan Solo daerah Ngawi Jawa Timur. 8th Ann.Tatanan stratigrafi dan posisi tektonik cekungan Jawa Tengah Utara selama Jaman Tersier. 30-38. p. 1. p. Kartanegara. 99.Early Pliocene in Kali Cilik section.Pliocene sediments. Indonesia. (IAGI). Kusumabrata. scale 1:100. O Sullivan & L. Late Miocene. Comparison between this study and palynology analysis indicates same climatic changes at Plio-Pleistocene boundary. p. (1999). Permana (2003). 1. Melbourne. Kapid. Bayah High and adjacent offshore areas. Hill. West Java. Petroleum Assoc. J. 13-41. Indonesia. Ciamis regency. 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Geol. 1-116. W. Jawa Timur. Asikin (1987). Overlying Totogan Fm clay breccia with various blocks with Late Eocene (NP 18-20) to Oligocene.Seismic survey in the North East Java Basin. p. 29-42. Koesoemadinata (1962). In: Proc. p. overlying Mundu Fm is upper NN12-NN14/ Early Pliocene) Kariyoso. Bandung. Java. 12 km N of Bojonegoro.Studi nannoplankton pada Formasi Karangsambung dan Totogan di daerah Luk Ulo.vangorselslist.T.T. Proc. 6. Kebumen. truncatulinoides. Pliocene or younger thrusting to N) Katili. Conv. C Java quadrangle with mainly folded Miocene. Southeast Asia (GEOSEA VI).De geologie en geomorphologie van Cheribon. overthrust by sheared.G. Open File Report E35-31. Previously exploited by Chinese for medicinal purposes) Kemmerling. Noble (eds.5 km NW of Rengel cave.Seismic reflection of the Sunda Trench in Eastern Java.C. ('Report on the occurrence of oil shale with therapeutic components (ichthyolt) in the Karangbolong Mountains. Klein. Kertapati. (1987). (W-most Java and Sunda Strait N-S trending half-grabens. Jakarta. granite. 94-100. Sediments possibly large blocks in melange.usgs.) Proc. Banjoemas (Kedu). Douglass). is source of subterranean river. Robinson. W Java'. M-L Miocene and Pliocene) Keil. red radiolarian chert.E. Geol. 305-310. p. p. K. 'lagoonal' fine tuffaceous rocks impregnated with bitumen. Geol. R. pyroxenite. Java). p. (1932). p. chaotic melange. Survey J. 259-269.F. Geol. Indonesia. T. (Earthquakes 1963-1983 show seismic zone dipping to N at 40°. K. K. 7. basalt. Suptandar & Wikarno (1976). also serpentinite and radiolarian chert and reworked Cretaceous Orbitolina limestone in Tertiary conglomerate. Serie 8 (Verbeek Volume). No details on age. gneiss. NW of Bandung. 342-361. 2.. River may be fed by water from sawahs of Grabagan. T.D.. quartzite and marble) and quartz porphyry with fission-track age of 65 Ma. 2. Verslagen Geol. 655-665. between andesite breccias. W. (IAGI). 5. Helvetiae 18. Int. (‘Description of two limestone caves near Bojonegoro. p. Eclogae Geol. U. Kastowo. Indonesia Geol. p. Sands contain no quartz.70°) Ketner.) Kisimoto. In: B.com Sept 2016 . Java’. Java). 305-322. Modjo. (online at: http://pubs.5 km from Nglirip village. Obradovich. Indon. p.L. Geol. with extension phases in Eo-Oligocene.vangorselslist.C. (online at: http://retro. J. Petroleum Assoc. Relatively constant dip of ~40° to S. (IPA). 1-10.B. or from possible absorbtion point 400m E of Manjung. R. 6th Regional Conf.W. E. (1915).Howes & R. BPM survey of thick (>3800m) exposed Tertiary sand-shale section in Ci Kao valley. phyllite with Rb-Sr age 85 Ma. faunas) Koch.Pre-Eocene rocks of Java. Serie 5.pdf) (Pre-Eocene of Lokulo area. G. Y. Verhandelingen Geologisch-Mijnbouwkundig Genootschap Nederland Kol. Res. 605-614. etc.gov/journal/1976/vol4issue5/report. Two large caves in Miocene coral-orbitoid limestone ('zone m3' of Verbeek) in NE Java. Surabaja. Assoc.) Proc. (1925). 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('Contribution to the stratigraphy of the Tagogapu.com Sept 2016 .0 62 www. (2009).vangorselslist.pdf) ('On a fossil tree trunk from Bolang. seismic tomography and geochemistry of arc volcanoes reflect horizontal slab tear in subducted Indo-Australian slab beneath Java segment of Sunda arc (105°E -116°E) at depth of 300-500 km. kugleri to above top Ga binaiensis (N6). 32nd Annual Conv. R. Jakovlev & B. Low-velocity anomaly in crust.(Local source tomographic inversion used to obtain 3-D models of crust and mantle wedge beneath C Java. Amsterdam. probably channels. 23p. 6. (online at: http://jurnal. 193-204. Masigit gebied (Noord Priangan. deemed to be new species named Dipterocarpoxylon javanense (= Dryobalanoxylon javanense according to Den Berger. Irawan & D. Apparently good planktonic foram age control from Top Gr. (New tomographic data from local seismicity. Jawa Timur. Apriadi (2003).ias. Crust and upper mantle velocity structure beneath C Java strongly anisotropic. H. (1941). Gahalaut (2011). Akademie Wetenschappen. Six sequences distinguished in open marine marls and limestone (calciturbidites?) in four outcrop sections in Rembang zone E of Tuban. just N of volcanic arc (MerapiLawu anomaly.Miosen bawah (P22.repository. I. p.Uber einen fossilen Baumstammm von Bolang (Java). In crust beneath middle part of C Java. HvG) Krausel. 1-31. P. 60 cm in diameter.lower N5) Kundu. R.Gamping.Gamping Fm. but they relatively common in some samples from Ciletuh Fm.E. 9. C Java’. Kristianto. Paris. Walat and Ciletuh Formations. Y. & H. (‘Nannofossil study of the claystone unit of Wungkal. Assoc. Walat and Ciletuh Fms M Eocene quartz-rich sequences in SWJava Basin.Sedimentary petrographic study of the Bayah. interpreted as lower shoreface to offshore environments. 309. Upward decrease in feldspars and volcanics and increase of polycrystalline quartz in some sequences consistent with uncovering of magmatic arc through erosion) Kusumastuti. Fanani & C. Indon. 1. Indon.edu. volcanic and sedimentary rocks.0 63 www. Indonesia. 1-114. Klaten. Prastistho & S. Porosity 25-35%. Sosromihardjo (2000).. 6.vangorselslist. (SW Java Eocene-Oligocene sandstones ‘recycled orogenic’ (sub-) litharenites. (IAGI). 195215. Bayat. 5p. S. 1. SE of Jakarta. 35th Conv. Discoaster saipanensis. Comptes Rendus Academie Sciences. In: Proc.Studi nanofosil pada satuan Batulempung. 27th Ann. Z. (Lapindo 1994 gas discovery in Pleistocene Pucangan Fm volcanoclastics in E Kendeng zone.uow.Sedimentology and stratigraphy of the Bayah.. Geol. granitic.deltaic.au/theses/1404/) (Bayah. 41-54. Provenance area to N or NE. (IPA). Conv. Twelve facies distinguished.A. Ciletuh Fm submarine fan. (IAGI). 17 gas sands between 500-3000’. Harjono (1989). Ph. based on seismic reflection data (Krakatau campaign)') Lehmann. In Indonesian) Kurniawan. 2012-E13.B. NSW. Boyolali. Reservoir geometries mainly sheet-like. SW Java basin.com Sept 2016 . quartz-rich 'recycled orogen' type) Kusumahbrata. Assoc. Ciletuh submarine fan mainly E to W paleocurrent directions? Provenance analysis suggest rel. 205-212.) Kurniawan.Analisa struktur dan stratigrafi terhadap keterdapatan rembesan minyak dan gas berdasarkan data permukaan di Formasi Kerek.The Wunut Field: Pleistocene volcaniclastic gas sands in East Java. (1994). Volcanic rock fragments rare in most samples from Bayah and Walat Fms.. Yogyakarta. H. Proc. Prasetyadi (2012). in fore-arc region of present Sunda Arc system. 23 rd Ann. Wonosegoro. (On structure. Assoc. B. stratigraphy and oil and gas seeps and outcrop data of Kerek Formation in W Kendeng zone. A. Many of seeps tied to faults) Kusumahbrata. Jakarta.Morphologische Studien auf Java. Bibliography of Indonesia Geology.B. dominated by various types of quartz and chert. barbadiensis. Proc. Murwanto (1994). Petroleum Assoc. Indon. p.Penentuan tektonogenesis komplek bancuh Karangsambung berdasarkan analisis kekar gerus. (online at: http://ro. 41st Ann. p.Extension crustale dans le detroit de la Sonde (Indonesie). Gas charge probably leakage from underlying Miocene Porong Reef) Kusumayudha. Surono. 1-253. 3. R. lintusan Watu Prahu. Proc. most reserves in deepest zone. Pekanbaru 2006. ('Crustal extension in Sunda Straits (Indonesia). O. Sulaeman. Conv. (1994). Cribrocentrum reticulatum. donnees de la sismique reflexion (Campagne Krakatau). Palaeocurrent data of Bayah and Walat Fm suggest sediment mainly derived from NNE. Geol. Formasi Wungkal. Seminar Geologi dan Geotektonik Pulau Jawa sejak Akhir Mesozoik hingga Kuarter.J. Closure formed in Late Pleistocene (gravity-driven detachment related to uplift in volcanic arc?). p. S of Surabaya. Huchon & H. W. Jawa Tengah. some patchy. etc. Conv.P. Proc. Ser. Bayah and Walat Fms fluvial. Suwarlan & S. D. Watuprahu section at Jiwo Hills SE of Yogyakarta contains Late Eocene nannofossil zones NP18-NP19 (incl. (IAGI). (Structural analysis of C Java Karangsambung-Luk Ulo melange and olistostrome complex) Lassal. Stuttgart.. Walat and Ciletuh Formations. Umiyatun (2006).D. p. Darmoyo. mounded geometry. Y. Boyolali area. C Java. 101-120. Ed. Geology Department Gadjah Mada University. A. p. Indon. Geol. Jawa Tengah. P. Thesis University of Wollongong. Geographische Abhandl.C. (1936).(Detailed sedimentological study of M Miocene Cibulakan Fm outcrops of glauconitic sands and shales along riverbed of Cipamingkis River. Southwest Java: its importance for interpreting provenance and petrographic correlation.. p. Analog of age-equivalent hydrocarbon zones in offshore NW Java Basins.I. Yogyakarta. probably derived from mix of metamorphic. Bayat. 11p. R. H. Jakarta. Reservoirs part of NE prograding volcanoclastic wedge from modern arc. Proc. Joint Conv.B. 2. structurally deformed and partly imbricated. In: R. Indonesia. Nanggulan Fm is transgressive sequence) Lelono. Studies in Geology 15. E. 355.E. Mainly on Southern Mountains SE of Yogya and NE Java KendengRembang zones around Cepu.shallow marine. p. (Two profiles across Java Trench P7 and N508 show subduction of Late Jurassic. J.go. Podocarpidites pollen in upper unit indicates cooling. 35. Scientific Contr. associated with substantial crustal thinning. 3. Compressional folding and basin inversion began in Late Miocene and appears to have been continuous into Recent time) Lelgemann.. Oil Gas. 45-80. P. S Sulawesi and Natuna. W. probably triggering submarine slides and turbidity flows. Offshore wells in forearc basin Oligocene volcaniclastics below base Miocene unconformity. G. in Late EoceneOligocene of wells in N Madura. 6. Royal Holloway. E. as these are generally first recorded in Early Miocene of other areas such as NW Java Sea. Generally poor pollen assemblages. Bakker.Active margins 3. Common brackish pollen of Zonocostites ramonae and Spinizonocolpites echinatus indicate mangrove/ back-mangrove environment) Lelono. p.Sea level changes during Middle-Late Eocene in the Nanggulan Formation. 3545-3548. Lemigas Scientific Contr. after collision of Australian plate and Sundaland in latest Oligocene. Spec. p.Transtensional basins in the western Sunda Strait.D. Ed. Gutscher. Reichert (2000).esdm. Bali.B.B. 1-457. 333-345. Uppermost portion of basement. Bibliography of Indonesia Geology. Individual imbrications may bend over toward trench in uppermost part. H.E Java Sea is unusual. (On crustal structure and evolution of Sunda Strait.Recent. Geophysical Res. Cottam & M.Palynological study of the Eocene Nanggulan Formation.E Cretaceous descending Indian Ocean crustt. (2001).) The SE Asian gateway: history and tectonics of Australia-Asia collision.Oligocene palynological succession from the East Java Sea. and 29th IATMI.a picture and work atlas. (2012).lemigas. (Unpublished) (Nanggulan Fm age diagnostic M-L Eocene fauna and palynomorph assemblages. P. Central Java. Weinrebe & C. Neogene transgressive-regressive cycle with basal marine sandstones and limestones. p.vangorselslist. 36th IAGI.B. Wilson (eds. Lelono. In: A. lacustrine elements rare. London. University of London. Many palynomorphs affinity with Indian forms. 14p. American Assoc.J. Thrusts steepening away from trench.. Lemigas.R. Unlike equivalent beds offshore NW Java. Doust. A. H. Introduction of term ‘cone-karst’) Lehner.(‘Geomorphologic studies on Java’. Soc. W Java. Thesis. suggesting plant migration into SE Asia following plate collision in E Tertiary. E. E.A. Bialas. Depositional environment transition non-marine. Ph. Publ. (2000). Guenau (1983). (Appearance of regular Gondwanan/ Australian pollen. (online at: www. Bally (ed. p. including Dacrydium and Casuarina.W. 1. Sediment fill of fore-arc basins Late Oligocene/E Miocene. M.id/ ) (Palynological studies of Oligocene in (unnamed) onshore wells in Ciputat sub-basin.Gondwanan palynomorphs from the Paleogene sediments of East Java?.com Sept 2016 . overlain by imbricated accretionary wedge of sediment. JCB2007-010. Distribution of similar M Eocene palynomorph assemblages suggests Sundaland extended from Java to SW Sulawesi. Transtensional character of the area shown by faulted blocks of arc basement and active normal faults on both sides of large graben at W entrance to Sunda Strait. 32nd HAGI. Morley (2011). E. S part of region 50 km from trench and Moho of downgoing plate is at depth of 28 km) Lelono. (AAPG). This may indicate earlier arrival of Gondwanan/ Australian fragment in East Java area than in other areas of Indonesia) Lelono. p. Flueh. Allenbach & J.) Seismic expression of structural styles. suggesting absence of lake deposit.0 64 www. the evidence of earlier arrival. Letters 27. S Sumatra and C Java. Geol. Petrol.Oligocene palynology of onshore West Java. probably equivalent to M-L Eocene boundary event recorded elsewhere. Geol. Oligocene defined by presence of Oligocene marker Meyeripollis naharkotensis. & R. Central Java. 8-15. M. 67-82. Over 6 km of graben fill sediment. Hall. Java Trench. Doming and fracturing of entire island arc region during Oligocene was followed by Miocene regional subsidence and tectonic quiescence. (2007). based on 1999 seismic survey.J. Reefs on unconformity indicates forearc basin subsided to present depth after Oligocene orogenic pulse. probably pillow basalts.B. E. South Central Java. p.Volcaniclastic controls on carbonate sedimentation within the Gunung Sewu area. Early part of Late Oligocene much reduced rain forest elements with grass pollen. (‘Contribution to the knowledge of Javanese volcanic rocks’) Bibliography of Indonesia Geology.. 70-113.com Sept 2016 .vangorselslist. Rotterdam. with volcaniclastic sedimentation from arc in N and carbonates from shallow platform to S. indicating more seasonal climate.W. suggesting more seasonal climate. 107-132. 1. Thesis Utrecht University.) (E Oligocene characterized by common rain forest elements. Bantam Residency. p. W Java Sea) Lelono. Wyt & Zonen. 34.esdm.Small foraminifera from the Late Tertiary of the Netherlands East Indies.The development of the Miocene Wonosari Formation. & R. 1-648. Sustained periods of volcaniclastic sedimentation resulted in decrease in species but increased numbers of individuals. West Java. 3. Doct. p.Oligocene palynological succession from the East Java Sea. S. Java. Lemigas Scientific Contr. Netherlands East Indies. N of carbonate platform deep (~200-400 m) fore-arc basin. Tectonics and sedimentation of Indonesia and 50th Anniversary Memorial of R. van Bemmelen’s Book. (1999). W Java) Lokier. Thesis. corals and other biota as tertiary elements. Some small foraminifera from the type locality of the Bantamien substage. 27 th Ann. (1941). Indon. p. suggesting everwet rain forest climate at that time. 95-104.J. (1944). (2000). S. rainforest climate. 2. (1879). Quarterly Colorado School Mines 36. L. (online at: www.lemigas.The Geology of Indonesia. whereas for latest Late Oligocene rain forest (and peat swamp) elements return in abundance. 6. Ed. Periodic inputs of marine volcaniclastics in carbonate environment. & R.B.id/id/pdf/scientific_contribution/. LeRoy. 1st FOSI-IAGI Reg. E of Pelabuhan Ratu. suggesting very wet rain forest climate) LEMIGAS/ BEICIP (1974). 3. Morley (2011). University of London. E. p. south area. p. (1999).W. L. Petroleum Assoc. 1-269. p.Miocene foraminifera from Sumatra and Java. p.(Palynomorph assemblages from independently dated marine Oligocene succession from E Java Sea wells here named X and Y. (M Miocene Wonosari/Punung Fm of south C Java active volcanic setting with carbonate development.W. lack of competitors and changes in substrate) Lokier.go. Early part of Late Oligocene much reduced rain forest elements.The Miocene Wonosari Formation. Jakarta.D. 217-222.id/id/pdf/scientific_contribution/…) (same paper as above) Lelono. Palynological succession similar to Sunda Basin. (Unpublished) LeRoy. Indonesia.go. suggesting everwet. Proc. Calcareous algae and larger foraminifera packstone dominate.Geology of the Kendeng zone (Central and East Java). p. Morley (2011). (Unpublished) (Regional study of Middle Miocene Wonosari Limestone in Southern Mountains of C and E Java) Lorie. Small foraminifera from the Miocene of West Java.B.. 50 (Abstract only) Lokier. Lemigas Scientific Contr. Seminar. suggesting superwet climate. Early Oligocene with common rain forest elements. (Descriptions of 107 species of small benthic foraminifera from Miocene marls at Tjijarian bridge. (online at: www. Quarterly Colorado School Mines 39. Bodjong beds. 2. Ph.W. S of E Miocene island-arc a moderate to high-energy carbonate platform developed. and presence of regular Gramineae pollen. Conv. E. 34. Netherlands East Indies.0 65 www. Some interdigitation of sediment types.esdm.lemigas. Indonesia: volcaniclastic influences on carbonate platform development. In latest Late Oligocene rainforest elements return in abundance.W. S.J.Oligocene climate changes of Java.W. 169-176. (IPA). Proc. 3. J. attributed to increase in nutrients.Bijdrage tot de kennis der Javaansche eruptiefgesteenten. South Central Java. (4) Late Oligocene. Survey Indonesia. possible effect of 18 Ma S Central Kalimantan uplift. Conv.. Petroleum Assoc. C. NN4) immature erosional products of metamorphic basement. (3) Early Oligocene half-graben extension. A. P.E.D. 13p. (5) 20-12 Ma tectonically quiescent. (‘The crystalline schists on Java are older than Cretaceous’. In: N. Lunt. not wrench-controlled. 39-72. (IAGI).I.Geology and exploration for low sulfidation epithermal gold-silver mineralization in Kerta. p. (Unpublished Sagaranten sheet of 1:100. P. J. (6) M Miocene/12 Ma fault inversion/ widespread subsidence phase.E Miocene Old Andesite volcanic arc in S Java. through 45° (150. 1340. Indon.com Sept 2016 . (1934). 352). O. simultaneous with widespread carbonates in N Java.000. P. Koulakov. Jakarta. compressional structures with application to Southeast Asia. Sahara (2013). & J. Basuki (ed. Brotopuspito.. S. Publ. 26-36. p. but are in interbedded marl-limestone series ~20m above 'transgressive conglomerate ' with common quartz pebbles on top of chlorite schist. Ratdomopurbo. (Comprehensive book on Java Sedimentary Geology Major tectonic events affecting sedimentation: (1) Late Mesozoic accretion of Paternoster microplate. Detected strong anomaly beneath C Java is unique in size and amplitude. Rabbel. I. P. 15 Ma is max. Geol. Sumbing. so not much left?. W. Ludwig. (2013). Assoc. 2. Herryurianto (2012). Zschau. Econ.P.vangorselslist.000. apparent product of a mid-Early Miocene orogenic event. some unusual aspects of stratigraphy. radiolarian chert and Eo-Oligocene sediments.De kristallijne schisten op Java ouder dan Krijt. Proc. HvG)) Lowell. Beds consistently and steeply S-dipping. probably isoclinally folded. Indonesian Soc. Rembang Line is N edge of accreted ‘Woyla Terranes’. (MGEI) Ann. De Mijningenieur 7.G. 20/21 Ma marks end of ‘Old Andesite’ volcanism. p. p.250 km). (1991). 2012. scale 1:100. Zwierzycki (1926). Toelichting bij blad 30 (Poerwakarta). Conv. Sumatra Pungut and Tandun oil fields do have indications of wrenching) Lubis. Batavia. 6. (7) Late Miocene/ 8 Ma: inversion of ‘Woyla terranes’. 1-45. p. (3D seismic velocity structure of Merapi volcano provided image of lithosphere and subduction zone beneath C Java. p. O. 261.Fluid ascent and magma storage beneath Gunung Merapi revealed by multi-scale seismic imaging.Explanatory notes of Sheet 30. C Java.0 66 www. Dienst Mijnbouw Nederlandsch-Indie. Banten. J. Spec. Singapore. Very different from M Miocene Ngrayong Fm mature quartz sands) Lunt. flood over Sundaland.Geologische kaart van Java 1:100. AAPG Bali 2000 Int.The Neogene geological history of East Java.Wrench vs. (2000). (Example from NE Java basin oil field structures: look compressional. but no clear backarc basins. (limestones being quarried for limestone kilns. Explanatory note to Sheet 26 (Sagaranten). Prihatmoko & Y. Proc. 7-19.A draft review of the Lutut Beds in the type area. and Lawu are located at edge of large low velocity body that extends from upper crust to upper mantle beneath C Java.000 geologic map of Java) Luehr. (Lutut sands from thrust belt SW of Semarang are Early Miocene (N6-N7. (IPA). Geol. to 70° (> 250 km). This segment of arc has high magma flux) Lunt. main phase Rembang-Madura-Kangean zone uplift. Mid-Cretaceous limestones with Orbitolina concavata near village of Karang Tengah in Loh Ulo river area. SEAPEX V. H. Banda and Eastern Sunda arcs. 63-70.S. (1980). Indon.) Proc. ('Geological map of Java 1:100. (2) MidEocene onset of sedimentation.000. Geol. are not intercalated with serpentinite and chlorite schist as argued by Verbeek & Fennema (1896. Ed. p. (8) mid-Pliocene-Pleistocene thrusting episodes) Bibliography of Indonesia Geology. K.The sedimentary geology of Java. 22-25. (1933). p. Conv. Malang. Purwakarta') Ludwig. J. Dip of subducting slab steepens from nearly horizontal (0-150 km from trench).Geological map of Java. 20th Ann.. B. Schists at higher levels and thrusted over Cretaceous sediments (from S to N). J. Fauzi & D. Active volcanoes of Merapi. Volcanology Geothermal Res./ IPA fieldtripappendix.Loth. Burgon & A. J. possibly latest Eocene. Huffman (1998).Indonesian Petroleum Association East Java geological field trip guide book. TD 340m. Kalan (1996). Dev. G. Indonesia. Pseudorotalia indopacifica basal occurrence near base zone N20) Mahfi. Sugiatno (2007). 247-258.Lunt. Sugiatno & T. P.The Pemali Formation of Central Java and equivalents: indicators of sedimentation on an active plate margin. Selorejo and Lidah Fms.F. P. 100-113. Kab. & S.6 ± 4.vangorselslist.Late Eocene clastics overlain by ‘middle’ Oligocene deep marine Tegalsari marls. Ed. (C Java clastics sections near Bumiayu with record of intra-Late Miocene/ ~7 Ma tectonic event) Lunt. (IPA) Fieldtrip Guidebook. Sag phase Oligo-Miocene carbonates show complex distribution. M. Netherwood & O.The Bagelen Beds. Conf. Jawa Tengah. Res. Paleolatitude determinations: Bayat Eocene limestone -22. (IAGI). 12. 11p.com Sept 2016 . H. P. overlain by Late Oligocene-Early Miocene ‘Old Andesites’) Lunt.Biodatum dan zonasi foraminifera bentik kecil serta hubungannya dengan foraminifera planktonik Sumur-95 daerah Cepu.. Central Java. Indon. (1984). Santa Barbara.the role of classic geological skills in 21st century exploration. Asian Earth Sci. 1-186. IPA Field Trip Guidebook. ('Datum levels and zonation of smaller benthic forams and their relations with planktonic foraminifera in well 95. Shallow well W of Cepu. Sumber Daya Geologi 17. M. C. Geol. P.Citarum area. Fuller 1999.From normal to oblique subduction: tectonic relationships between Java and Sumatra. Kalissongo and Karang Sambung show mixture of rotated and unrotated sites.0 67 www. p. 29th Ann. (Examples of application of classic geology in hydrocarbon exploration on Java. very deep marine ‘scaly’ clay olistostrome deposit. Assoc.. Schiller & T. Zen (1995). 1-2. South Central Java. Blora. Petroleum Assoc. Bibliography of Indonesia Geology. Bandung (in press?). 34p. J. 5 (161).A report on fieldwork in the Rajamandala.A paleomagnetic study of Miocene and Eocene rocks from Central Java. (Unpublished Manuscript) (Rajamandala Limestone Late Oligocene age.State of the art or state of decay?.. J. West Java.9 ± 9 °S. (Unpublished report) Maha. Burgon (2003). Yogya Oligo-Miocene basalt -11. 1998. Sanyoto (2000).. Geol. Kulunprogo Oligo-Miocene andesite -8 ± 2 °S)) Malod. 34. Allan (2000).A review of the Lutut Member in the type Area. suggesting local tectonic controls more important than assumed eustatic trends) Lunt. J. Mountains.A. p. Singapore April 2003. 336356. Sugiatno (2003).. P. Cepu area. (Unpublished) (Paleomagnetic results from Bayat. & G. A. (Bagelen Beds of C Java ~10 km N of Lok Ulo are basal Oligocene (~32. Calcarina calcar restricted to Pleistocene (planktonic foram zones N22-N23). & H. 85-93. (Details on Karangsambung. 1-63. Thesis. p. Karta.IPA Field Trip to Central Java. 6. similar to Lok Ulo.5 Ma). SEAPEX Expl. P.. p.A. Java'. p.T. 4.3°S. Southeast Asian Earth Sci. penetrating Late Pliocene. p. & H.O.A review of the Eocene and Oligocene in the Nanggulan area. University of California. Sugiatno (2007). probably with blocks of M Eocene (Ta) nummulitid limestone. Baky (2009). Kendeng zone and Rembang zone outcrops descriptions) Lunt. Underlying quartz-rich clastics are Early Oligocene in age) Lunt. Indon. M. Early Miocene sediments show major tectonic event during quiet sag phase of previous workers.Pleistocene Mundu. Proc. Mix of basement and Eocene boulders in Sangiran Domome possibly from underlying similar E Oligocene olistostrome) Lunt. 1-57.M. P. Baturagung/ Jiwo Hills and Sangiran Dome outcrops) Lunt. p. R. Centre (GRDC). North Central Java. D. Beslier & M. Conv. K. & H. 27p. (S. (Unpublished) (Middle. P. (Oblique subduction beneath Sumatra induces strike-slip faults in Sumatra. Subduction perpendicular to trench SW of Java. Cimandiri FZ of W Java continues out to sea. Sinistral activity on land may be conjugate of dextral strike-slip along NW-SE prolongation of Sumatra strike-slip fault in forearc. Structural transition is S of Pelabuhan Ratu Gulf. To W, oblique subduction induces partitioning into convergent motion and NW strike-slip motion. To E subduction is normal and typical forearc basin develops) Mandang, Y.I. & N. Kagemori (2004)- A fossil wood of Dipterocarpaceae from Pliocene deposit in the West region of Java Island, Indonesia. Biodiversita 5, 1, p. 28-35. (Online at: www.unsjournals.com/D/D0501/D0501pdf/D050106.pdf) (Giant silicified dipterocarp tree trunk 28 m long from Lower Pliocene near Leuwidalang, Banten, W Java, described as Dryobalanoxylon lunaris) Mandang, Y.I. & D. Martono (1996)- Keanekaragaman fosil kayu di bagian barat pulau Jawa. Bul. Penelitian Hasil Hutan 14, 5, p. 192-203. ('Fossil wood diversity in the western part of Java Island'. Of 199 wood fossils, 81% belong to family Dipterocarpaceae (Dryobalanops, Alstonia, Calophyllum, Dillenia, etc.)) Manga, M. (2007)- Did an earthquake trigger the May 2006 eruption of the Lusi mud volcano? EOS 88, 18, p. 1 Mannhardt, F.G. (1920)- Rapport over het voorkomen van asphalt- en phosphaat-afzettingen aan den voet van het Kromong-gebergte, in het District Palimanan der residentie Cheribon. Jaarboek Mijnwezen Nederlandsch Oost-Indie 47 (1918), Verhandelingen 1, p. 9-18. (‘Report on the occurrence of asphalt and phosphate deposits at the base of the Kromong Mountains, Palimanan District, Residency Cirebon’. Four small asphalt deposits/ oil seeps in Miocene limestone ~20 km W of Cirebon, just SW of Palimanan village, known since Verbeek & Fennema 1896. Associated with hot springs and phosphate around Kromong/ Gunung Gundul andesite plug. With 1:20,000 scale map. Stratigraphy description see Harsonon Pringgoprawiro et al (1977)) Mansfeldt, H.A. (1876)- Verslag over een onderzoek naar den stand van de particuliere aardolie-ontgining in de Residentie Cheribon. Jaarboek Mijnwezen Nederlandsch Oost-Indie 1876, 2, p. 183-206. ('Report on an investigation of the private petroleum exploitation in the residency Cirebon'. Report on 1875 government geologist visit to first (minor) Java oil production W of Cirebon. Minor oil encountered here by Reerink in shallow 'Tjibodas' wells near Madja oil seep) Manurung, M. (1988)- Sulphide mineralization in the Gunung Limbung District, West Java, Indonesia. Ph.D. Thesis, University of Wollongong, p. 1-175. (Unpublished) Marcoux, E. & J.P. Milesi (1994)- Epithermal gold deposits in West Java, Indonesia: geology, age and crustal source. In: T.M. van Leeuwen et al. (eds.) Indonesian mineral deposits- discoveries of the past 25 years, J. Geochemical Exploration 50, 1-3, p. 393-408. (Epithermal gold mineralization in SW Java hosted by Miocene and Pliocene intrusions and volcanics. Most ore deposits of Bayah Dome related to extensive Pliocene magmatism dated as 5.7- 2.0 Ma. Mineral deposits localised by structural controls, in particular a strike-slip fault reactivated as normal fault. Lead isotopes suggest existence of underlying Precambrian crust in W Java) Marcoux, E., J.P. Milesi, T. Sitorius & M. Simandjuntak (1996)- The epithermal Au-Ag-(Mn) deposit of Pongkor (West Java, Indonesia). Indonesian Mining J. 2, p. 1-17. Marcoux, E., J.P. Milesi, S. Sohearto & R. Rinawan (1993)- Noteworthy mineralogy of the Au-Ag-W (Bi) epithermal ore deposit of Cirotan, West Java, Indonesia. The Canadian Mineralogist 31, p. 727-744. (Pliocene age (1.7 Ma) Cirotan Au-Ag ore deposit of Cikotok District, SW Java, producing since 1955. Considered as hybrid deposit transitional between low-level adularia-sericite epithermal type and porphyry-tin type of deposit) Bibliography of Indonesia Geology, Ed. 6.0 68 www.vangorselslist.com Sept 2016 Marks, P. (1956)- Smaller foraminifera from well No. 1 (sumur 1) at Kebajoran, Djakarta. Djawatan Geologi, Publ. Keilmuan 30, Seri Paleont., Bandung, p. 25-47. (Study of foraminifera in water well drilled to 255m in 1950 at S side of Jakarta. Mainly barren, non-marine section with 3-4 thin intervals with shallow marine microfauna (Asterorotalia, Pseudorotalia, Elphidium, etc.). Uppermost samples rich in reworked planktonic forams. Age of section latest Pliocene- Pleistocene) Marliyani, G.I. (2016)- Neotectonics of Java, Indonesia: crustal deformation in the overriding plate of an orthogonal subduction system. Ph.D. Thesis Arizona State University, p. 1-392. (online at: https://repository.asu.edu/attachments/170517/content/Marliyani_asu_0010E_16033.pdf) (Analysis of seismicity and active faulting on Java, particularly Cimandiri and Pasuruan Faults and volcano morphology) Martha, A.A., S. Widiyantoro, P. Cummnins, E. Saygin & Masturyono (2016)- Investigation of upper crustal structure beneath eastern Java. Proc. 5th Int. Symposium on earthhazard and disaster mitigation, AIP Conf. 1730, Bandung, 020011, p. 1-7. (Ambient Noise Tomography method used to detect structure under E Java. N Rembang zone, most of S Mountains zone, are areas of high gravity anomaly and high velocity zones. Kendeng zone and most of basin in Rembang zone associated with low velocity zones) Martin, K. (1879-1880)- Die Tertiarschichten auf Java, nach den Entdeckungen von Fr. Junghuhn, Palaeontologischer Teil (1879-1880). E.J. Brill, Leiden, p. 3-164. (‘The Tertiary beds of Java, after the discoveries of Fr. Junghuhn; paleontological part’. First of many Martin publications on Tertiary fossils from Java. With descriptions of many new species, incl. Cycloclypeus annulatus from Citarum valley, W Java. Chapter on corals p. 132-146, mainly from Miocene of Nyalindung area, W Java) Martin, K. (1880)- Revision of the fossil Echini from the Tertiary strata of Java. Notes from the Leyden Museum 2, p. 73-84. (online at: www.repository.naturalis.nl/document/551344) (Brief revisions of 19 species of echinoids originally described by Herklots (1854). Most of these are not new species as proposed by Herklots and many of them are still living today. No figures or locality information) Martin, K. (1880)- Untersuchungen uber die Organisation von Cycloclypeus Carp. und Orbitoides D'Orb.. Niederlandisches Archiv fur Zoologie 5, 2, p. 185-206. ('Investigations on the organization of Cycloclypeus and Orbitoides'. Early descriptions of MiocneJava larger foraminifera Cycloclypeus (C. annulatus, C. communis, C. neglectus) and Lepidocyclina (here still called Orbitoides; including new species radiata, carteri, gigantea)) Martin, K. (1881)- Tertiaerversteinerungen vom ostlichen Java, nach Sammlungen Junghuhn's und der Indischen Bergbeambten. Sammlungen Geol. Reichs-Museums Leiden, Ser. 1, 1, p. 105-130. (online at: www.repository.naturalis.nl/document/552410) ('Tertiary fossils from East Java, from collections of Junghuhn and Indies mining engineers'. Incl. descriptions of Eocene larger foraminifera Nummulites djokjokartae n.sp. and Discocyclina (Orbitoides dispansa) from Yogyakarta area, echinoids (Pleurechinus javanus, etc.), bivalves, gastropods, etc. With 4 plates) Martin, K. (1882)- Tertiaerversteinerungen vom ostlichen Java, nach Sammlungen Junghuhn's und der Indischen Bergbeambten. Jaarboek Mijnwezen Nederlandsch Oost-Indie 1882, Wetenschappelijk Gedeelte p. 253-280. ('Tertiary fossils from East Java, etc', Same as Martin (1881) paper above) Martin, K. (1883)- Nachtrage zu den 'Tertiarschichten auf Java', 1er Nachtrag: Mollusken, nach Sammlungen der Indischen Bergbeambten, Junghuhn's und Reinwardt's. Sammlungen Geol. Reichs-Museums Leiden, Ser. 1, 1, E.J. Brill, p. 194-270. (also in Jaarboek Mijnwezen Nederlandsch Oost-Indie 1883, Wetenschappelijk Gedeelte p. 285-358) (Continuation of ‘The Tertiary beds of Java', part 1, molluscs. Descriptions of 71 species) Bibliography of Indonesia Geology, Ed. 6.0 69 www.vangorselslist.com Sept 2016 Martin, K. (1883-1887)- Palaontologische Ergebnisse von Tiefbohrungen auf Java, nebst allgemeineren Studien uber das Tertiar von Java, Timor und einiger anderer Inseln. Sammlungen Geol. Reichs-Museums Leiden, Ser. 1, 3, p. 1-380. (online at: www.repository.naturalis.nl/document/552425) ('Paleontological results of deep wells on Java, and more general studies on the Tertiary of Java, Timor and some other islands'. Descriptions of Tertiary fossils from outcrops and from water wells on Java (Grissee (=Gresik?)- NE Java, Batavia, Ngembak- W of Purwodadi), mainly collected by Van Dijk of Geological Survey. Mainly on gastropods and bivalves, also fish teeth, crabs. With 15 plates) Martin, K. (1883)- Palaontologische Ergebnisse von Tiefbohrungen auf Java, nebst allgemeineren Studien uber das Tertiar von Java, Timor und einiger anderer Inseln- 1. Jaarboek Mijnwezen Nederlandsch Oost-Indie 12 (1883), Wetenschappelijk Gedeelte, p. 371-412. ('Paleontological results of deep wells on Java, and more general studies on the Tertiary of Java, Timor and some other islands'. Part 1 of Martin (1883) paper above) Martin, K. (1884)- Palaontologische Ergebnisse von Tiefbohrungen auf Java, nebst allgemeineren Studien uber das Tertiar von Java, Timor und einiger anderer Inseln- 2. Jaarboek Mijnwezen Nederlandsch Oost-Indie 13 (1884), Wetenschappelijk Gedeelte, p. 77-216. ('Paleontological results of deep wells on Java, and more general studies on the Tertiary of Java, Timor and some other islands'. Part 2 of Martin (1883) paper above) Martin, K. (1885)- Palaontologische Ergebnisse von Tiefbohrungen auf Java, nebst allgemeineren Studien uber das Tertiar von Java, Timor und einiger anderer Inseln-3. Jaarboek Mijnwezen Nederlandsch Oost-Indie (1885), Wetenschappelijk Gedeelte, p. 5-108. ('Paleontological results of deep wells on Java, and more general studies on the Tertiary of Java, Timor and some other islands'. Part 3 of Martin (1883) paper above) Martin, K. (1887)- Palaontologische Ergebnisse von Tiefbohrungen auf Java, nebst allgemeineren Studien uber das Tertiar von Java, Timor und einiger anderer Inseln-4. Jaarboek Mijnwezen Nederlandsch Oost-Indie (1887), Wetenschappelijk Gedeelte 2, p. 253-342). ('Paleontological results of deep wells on Java, and more general studies on the Tertiary of Java, Timor and some other islands'. Part 4 of Martin (1883) paper above) Martin, K. (1891)- Die Fossilien von Java, auf Grund einer Sammlung von R.D.M. Verbeek und von anderen, Band I, Gasteropoda. Sammlungen Geol. Reichs-Museums Leiden, N.F., 1, 1-2, p. 1-132. (online at: www.repository.naturalis.nl/document/552454) (Reprinted in Jaarboek Mijnwezen Nederlandsch Oost-Indie 1896, Wetenschappelijk Gedeelte, p. 43-328) ('The fossils of Java, based on a collection of R.D.M. Verbeek'. Firsst of series of papers by Martin and collaborators on fossils of Java, published between 1891-1922. Volume 1 mainly extensive taxonomic descriptions of Tertiary gastropods. With 20 plates) Martin, K. (1891)- Die Fossilien von Java, auf Grund einer Sammlung von R.D.M. Verbeek, Mollusken Heft 57. Sammlungen Geol. Reichs-Museums Leiden, N.F., 1, 1-2, p. 133-332 (online at:www.repository.naturalis.nl/document/552458) (Second continuation of Martin (1891) monograph on Tertiary gastropods of Java. Includes 19 species of Turritella, also Purpura, Triton, Acanthina, Ranella, Cassis, Strombus, Potamides, etc.. With 45 plates) Martin, K. (1891)- Die Foraminiferen fuhrenden Gesteine, Studien uber Cycloclypeus und Orbitoides. Appendix in Die Fossilien von Java, auf Grund einer Sammlung von R.D.M. Verbeek, Sammlungen Geol. Reichs-Museums Leiden, N.F., 1, p. 1-12. (online at: www.repository.naturalis.nl/document/552466) ('The foraminifera-bearing rocks- Studies on Cycloclypeus and Orbitoides'. Early summary paper on W, C and E Java larger foraminifera (mainly species of Cycloclypeus)) Bibliography of Indonesia Geology, Ed. 6.0 70 www.vangorselslist.com Sept 2016 Martin, K. (1895)- Neues uber das Tertiar von Java und die mesozoischen Schichten von West-Borneo. Sammlungen Geol. Reichs-Museums Leiden, E.J. Brill, ser. 1, 5, 2, p. 23-51. (online at: www.repository.naturalis.nl/document/552400) ('News on the Tertiary of Java and the Mesozoic beds of West Borneo'. Mainly listings of Tertiary gastropods from various localities of Java. No maps, no illustrations) Martin, K. (1900)- Die Eintheilung der Versteinerungs-fuhrenden Sedimente von Java. Jaarboek Mijnwezen Nederlandsch Oost-Indie (1900), 108 p. ('The classification of the fossiliferous rocks of Java' Overview of fossils and discussion of probable ages of formations from various parts of Java and Madura. Very 'wordy'; no maps, tables or other illustrations) Martin, K. (1900)- Die Eintheilung der Versteinerungs-fuhrenden Sedimente von Java. Sammlungen Geol. Reichs-Museums Leiden, Ser. 1, 6, p. 135-244. (online at: www.repository.naturalis.nl/document/552390) ('The classification of the fossiliferous rocks of Java' Same paper as Martin (1900)) Martin, K. (1907)- Eine Altmiocane Gastropodenfauna von Rembang, nebst Bemerkungen uber den stratigraphischen Wert der Nummuliden. Sammlungen Geol. Reichs-Museums Leiden, Ser. 1, 8, p. 145-152. (online at: www.repository.naturalis.nl/document/552421) (‘An Early Miocene gastropod fauna from Rembang, with comments on stratigraphic value of nummulitids’. Listing of 40 gastropod species from Sedan and Gunung Butak, Rembang District, NE Java, only 6 species still known from recent faunas. Fauna held for Early Miocene (but associated with Cycloclypeus annulatus, so more likely Middle Miocene age, probably Bulu Limestone; HvG). No figures) Martin, K. (1907)- Systematische Ubersicht uber die Gastropoden aus Tertiaren und jungeren Ablagerungen von Java. Neues Jahrbuch Mineral. Geol. Palaont. 1907, 2, p. 151-162. ('Systematic overview of Tertiary and younger gastropods from Java'. Listing of 648 gastropod species names. No illustrations, ranges, descriptions, etc.) Martin, K. (1908)- Das Alter der Schichten von Sonde und Trinil auf Java. Verslagen Kon. Nederl. Akademie Wetenschappen Amsterdam, Afd. Wis. Natuurk., 17. p. 7-16. ('The age of the Sonde and Trinil beds on Java') Martin, K. (1909)- Die Fossilien von Java, auf Grund einer Sammlung von R.D.M. Verbeek, Lamellibranchiata. Sammlungen Geol. Reichs-Museums Leiden, N.F., 1, 2, p. 333-386. (online at: www.repository.naturalis.nl/document/552467) (Second continuation of Martin (1891) monograph on Java Tertiary fossils:. Tertiary bivalves, incl. Ostrea, Placuna, Pecten, Arca, etc. With 12 plates) Martin, K. (1911)- Enkele beschouwingen over de geologie van Java. Verslagen Vergadering Kon. Nederl. Akademie Wetenschappen, Amsterdam, Afd. Wis. Natuurkunde, p. 19-23. ('Some considerations on the geology of Java'. Observations from Martin's 1910 travels in Priangan and Yogyakarta area) Martin, K. (1911)- Vorlaufiger Bericht uber geologische Forschungen auf Java- 1 Teil. Sammlungen Geol. Reichs-Museums Leiden, E.J. Brill, Ser. 1, 9, 1, p. 1-76. (online at: www.repository.naturalis.nl/document/552384) (‘Preliminary report on geological investigations on Java- part 1’. Includes chapters on geology and fossils of Preanger (1: Nyalindung (p. 5-24), 2. Kalksteine von Radjamandala: ‘Old Miocene’ Rajamandala limestone with Alveolina, Heterostegina many Lepidocyclina (p. 24-29), and Yogyakarta areas (p. 56-76)) Martin, K. (1912)- Vorlaufiger Bericht uber geologische Forschungen auf Java- 2 Teil. Sammlungen Geol. Reichs-Museums Leiden, Ser. 1, 9, 1, p. 108-200. Bibliography of Indonesia Geology, Ed. 6.0 71 www.vangorselslist.com Sept 2016 with some gastropods of Eocene affinity. Mitra. (1916).Scaphopoda. 103 species.1158. General part. B. Flosculinella globulosa. B. 2. 3. one near Nanggulan with E Miocene Miogypsina and Lepidocyclina and one just W of Yogyakarta. Geol.Die Fauna des Obereocans von Nanggulan auf Java. Gastropods’. K. 7. Scaphopoda.nl/document/552451) (‘The Early Miocene fauna of the West Progo Mountains on Java. Reichs-Museums Leiden. p. ('Further considerations on the geology of Java' Mainly on Eocene. (1912). N.naturalis. Ed.naturalis.naturalis.Die Altmiocane Fauna des West-Progogebirges auf Java. Lamellibranchiata. 6.Verdere beschouwingen over de geologie van Java. No illustrations)) Martin. Akademie Wetenschappen Amsterdam. with introductory remarks on the geology of the island'. K. Descriptions of very well. 4-5.naturalis. A. Lamellibranchiata. D.(online at: www..nl/DL/publications/PU00012270. with descriptions of shallow marine fossil assemblages of E-M Miocene of S Mountains. Natuurk. 161173. Lamellibranchiata.. with Nummulites. Orthophragmina (= Discocyclina). Reichs-Museums Leiden. Wis. 20. ('Some general considerations on the Tertiary of Java'.Ngampel. p. 6. Includes chapters on (1) folded Eocene beds of Kali Puru nearNanggulan.knaw. Afd.pdf) (Rich Miocene macrofossils from right bank of Progo River. etc. Scaphopoda (Dentalium). Sammlungen Geol. only 7% still alive today. D.dwc. Early overview of Cretaceous. Brill. p. (1919). still some shine and color). Sammlungen Geol. (online at: www. Rundschau 4. ser. (1914). p. Akademie Wetenschappen. (online at: www. (online at: www. Early overview of Java stratigraphy. Proc. Continuation of Martin (1916). Scaphopoda. 1-158. C.Einige allgemeinere Betrachtungen uber das Tertiar von Java. 108 species of gastropods and molluscs and overlain by andesites.. K. Kon. 1151. K. Rhizopoda (larger forams Miogypsina thecidaeformis.).repository.(2) two 'Gunung Gamping' limestone hills.Die Altmiocane Fauna des West-Progogebirges auf Java. K.F.repository. Cycloclypeus. Verslagen Kon.repository. A. (1913).preserved fossils from classic U Eocene locality of Nanggulan.0 72 www. Cardium. D. Leiden. K. Foraminifera'.Unsere palaeozoologische Kenntnis von Java mit einleitenden Bemerkungen uber die Geologie der Insel. Orbiculina)) Martin. p.F. ('Our paleozoological knowledge of Java. 800-804. D. C. Nummulites djokdjokartae. Gastropoda. 261-296. Shallow marine Indo-Pacific mollusc assemblage.(3) localities in Rembang zone Ngandang.vangorselslist. Amsterdam.nl/document/552451) (‘The Early Miocene fauna of the West Progo Mountains on Java. N.com Sept 2016 .On the Miocene fauna of the West Progo Mountains in Java. Chapters A. etc. (online at: www. p. from E Miocene SW of Yogyakarta) Martin. C Java’. 223-261. Reichs-Museums Leiden. fritschi) and E. Rhizopoda.repository. Most likely age Early Miocene) Martin. 107-222. 6.Recent fossils of Java and introduction to Java geology.nl/document/552391) (‘Preliminary report on geological investigations on Java. Potamides. Tertiary mollusc species in Bibliography of Indonesia Geology. Nederl. Conus. 2. with widespread M Miocene Cycloclypeus annulatus limestones and 72 species of gastropods. Discocyclina dispansa. W of Yogyakarta.nl/document/552460) (‘The fauna of the Upper Eocene of Nanggulan. pengaronensis. Main localities: marls at Gunung Spolong and clay Kembang Sokkoh (well preserved. N. 2. Lamellibranchiata (Arca. SW of Yogyakarta:B.part 2’. Gastropoda. W of Yogyakarta. with ages of formations dated by percentages of Recent mollusc species) Martin. of possible Miocene age. Sammlungen Geol.Miocene rocks and fossils around Yogyakarta. p. C. With 8 plates) Martin. (1918). Rhizopoda (foraminifera incl. (1917). Associated with Miogypsina thecidaeformis. Lepidocyclina. (4) Pliocene beds of Candi near Semarang) Martin. K. J. (‘The molluscs of the Nyalindung Beds. 4 p. Gasteropoda. (1931). J. ('Pliocene fossils from Cirebon in Java'. Descriptions of molluscs from fossil-rich claystones of M -L Miocene Nyalindung Beds of Priangan. suggesting absence of open-sea connection between Far East and Europe as far back as Late Eocene) Martin. K. locality descriptions) Martin. Van der Vlerk and Gerth. K. p.F.The age of the Tertiary sediments of Java.M.Die Mollusken der Njalindungschichten. (1926). 3. Additions to Martin (1919) paper. Scaphopoda. Lamellibranchiata. ('Molluscs from the Upper Eocene of Nanggulan'. Verhandelingen 3. Leidsche Geol. Follow-up of Martin 1915 paper.repository. Sammlungen Geol. 754-765. General Part') Martin. K.D. SW Java. Brill. p. 3. Leiden.Eine Nachlese zu den neogenen Mollusken von Java. C Java.Indonesia different from Paris Basin and other European localities. p. No maps or stratigraphy info) Martin. 2. 471-496. 1. Sammlungen Geol.naturalis.naturalis. Lamellibranchiata. Geol. Serie9. Gastropods'. (online at: www.) Bibliography of Indonesia Geology.nl/document/552465) (‘The molluscs of the Nyalindung Beds. Leiden. part 1. Cosijn opgenomen antiklinaal in de residentie Surabaja. Mededelingen 3. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederlandsch-Indie 20. 162 species of gastropods and bivalves with living species ~15%. collected by Zwierzycki. Nyalindung Beds (W Java) and Tjilanang Beds. (1932). Scaphopoda. suggesting age no older than Late Pliocene. Proc. (1922). Ed. Cosijn'.. (N. 1-56. First Pan-Pacific Science Congress. surveyed by J. 72 new species. suggesting E Miocene age) Martin. No stratigraphy. 149-151. based on new MiocenePliocene mollusc material collected by Geological Survey in W Progo Mts (C Java). ('An Eocene nautilus from Java'. Gastropoda (continuation). Bishop Museum. K.com Sept 2016 . K. (online at: www. p. K. New Nautilus species from Eocene of Kali Puru.. SW of Karang Suwung) Martin. 4. p.Die Mollusken der Njalindungschichten erster Teil. Martin. p. Allgemeiner Theil. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederlandsch-Indie 18. of which 68% still extant. 1-24. 105-129. Verhandelingen Geologisch-Mijnbouwkundig Genootschap Nederland Kol. (1928).vangorselslist. 7. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederlandsch-Indie 4.Ein eocaner Nautilus von Java. In: Die Fossilien von Java auf Grund einer Sammlung von Dr. R. 2. p. (1932). Brill.nl/document/549774) ('Supplement to the Neogene molluscs from Java'.) 1. Shallow marine and brackish water molluscs from Pliocene of Tji Doerei.De ouderdom der sedimenten van den door Dr. Nanggulan.F.Bericht over fossielen van Kedoengwaroe in Soerabaja. C Java. 128 species of molluscs at Kedungwaru.J. Bernice P. Reichs-Museums Leiden. Jaarboek Mijnwezen NederlandschIndie 59 (1930). ('Report on fossils from Kedung Waru in Surabaya'. 6. ('The age of the sediments of the anticline S of Surabaya. Verbeek und von anderen bearbeitet durch Dr. Spec. E. E.repository. 113-121. K.Mollusken aus dem Obereocaen von Nanggulan. K. Martin's final paper?) Martin. 446-496. Shallow marine Pliocene molluscs from Kedung Waru anticline along road Jetis-Sidoteko) Martin. K. Honolulu 1920. Reichs-Museums Leiden.0 73 www. Gasteropoda (Fortsetzung). Publ. p. Martin. (1932). K. 3. (1921).Plioceene versteeningen van Cheribon in Java. Taxonomic descriptions of molluscs (mainly gastropods) from the shallow marine Upper Eocene of Nanggulan. N. (1921). 21st Ann. (Unpublished) (3-day fieldtrip to Eocene-Oligocene outcrops at Bayah. (IAGI). Geol. W Java. 29-38. Assoc.. Engelmann. IAGI Conv. & Y. 15th Ann. 362369. (1989). (Eocene. W Java'. incl. W Java. West Java. Indon. Doct. Petroleum Assoc. 2.Oligocene Ciletuh Fm of SW Java has lower slope characteristics and conformably overlies melange complex) Martono. In: L. S. Martodjojo.. Blanckenhorn (eds. S. In: Proc. Located N of S Serayu Mts with famous Luk Ulo melange.P. S. Publ. Res.Paleogene sequence stratigraphy South West Java.Die fossilen Gastropoden. Teknologi Bandung. Bandung 2003. Indon. Workshop Stratigrafi Pulau Jawa. Bandung. Hadiwisastra (1978). 6th Regional Conf. p. 30.) Die Pithecantropus-Schichten auf Java. 1-238. Indon. Geologi Indonesia (J. p. Jawa Barat. (1911). Geol. 46-51. SW of Bandung. Geol. Bull.-IAGI) 12. (1995). M Miocene tuffs) Martodjojo.Geologi struktur pegunungan Serayu Utara. 229-244. IAGI. p. p. Conv. p. Martodjojo. (2003). S. Jawa Barat. S. Geologi Indonesia 5. H. & Djuhaeni (1989).Martin-Icke. (2004). (Eocene-Recent stratigraphy and tectonic evolution of the Bogor Basin. p. Martodjojo. the Bogor Basin. Ed.0 74 www.H.Darmawisata IAGI 1981 ke daerah proyek Saguling. Shifing of arc from N to S left all of Java as basin. 1. Martodjojo.com Sept 2016 . ('Geologic structure of the North Serayu Mountains'. ITB Press. June 1987. Dev.Evolusi Cekungan Bogor. Koesoemo (1993). 31 p. Centre (GRDC).E Miocene in S (Indian Ocean) and modern arc along axis of Java. see also Martodjojo 2003) Martodjojo. Geology Mineral Hydrocarbon Resources of Southeast Asia (GEOSEA VI). 1-30. Selenka & M. Suparka & S. (1986).Early Pleistocene fossil gastropods from Trinil. S. (Three magmatic arcs in Java: Cretaceous. Conv. Cibadak) Martodjojo. Thesis Inst.Stratigrafi daerah Majalengka dan hubungannya dengan tatanama satuan lithostratigrafi di Cekungan Bogor.Sea level changes and tectonism causes and responses between stable Rembang and active Kendeng Zones. Jakarta 1987. Petroleum Assoc. In: B. (IPA). Jakarta. Situmorang (ed. (Fieldtrip guide with geologic summary Saguling Dam area. Res.Stratigrafi Pulau Jawa “state of the art”. Spec.PT Stanvac Indonesia West Java field trip. 1-55. 6. Episodic basin subsidence related to periodic loading by thrust sheets) Martodjojo.Cibinong and Gunung Walat. Bandung. Geol. p.) Proc. Bogor Trough. (1984). Assoc.Status Formasi Ciletuh dalam evolusi Jawa Barat.Evolusi Cekungan Bogor. (1987). Unrevised printed edition of 1984 thesis by Penerbit ITB Bandung) Martodjojo. p. S. Pre-Symposium Fieldtrip. (1992).Eocene in N (Java Sea). S. Dev. M Oligocene.vangorselslist. p. p. fieldtrip. Proc. Miocene turbidite fans in Bogor Basin progressively younger to N. S. 9-19.Recent geological events) Bibliography of Indonesia Geology. collected by Selenka expedition) Martodjojo. Central Java. 15. Centre. (Late Pliocene . N Serayu mountains nearly complete record of Eocene. S. Leipzig. U. (Stratigraphy Majalengka area. Gunung Walat. underlain by Cretaceous-Eocene accretionary crust and backarc basin during most of Tertiary. W Java) Martodjojo. 227-252. Bandung.Stratigraphic and tectonic behaviour of a back arc basin in West Java. ('Evolution of the Bogor basin. 396 p. Geologische und palaontologische Ergebnisse der Trinil-Expedition (1907 und 1908). Sujono (1981). S. Indone. Ciletuh. Post-Convention Fieldtrip. Sreymean. W of Wates.bgl.bgl. (online at: http://ijog. (2015).forereef slope facies. Milsom.Mineralization environment of the metamorphic rock-hosted Au prospect at Kebutuhjurang.com Sept 2016 . S. Petrography of Miocene limestone in Ngrijang Sengon section in Gunungsewu geopark region) Masson. ('Limestone sedimentology of the Jonggrangan Formations along the Kiskendo Cave section. J.G. K. Citatah. p. Dwiyanto & H.Sedimentologi dan diagenesis batugamping Formasi Wonosari di Ngrijang Sengon.reef flank facies with several reef core facies) Maryanto. Lunt 2013) Maryanto.vangorselslist. Geologi Sumberdaya Mineral 16. Boyce (2011). Jawa Timur. 6.Perkembangan sedimentologi batugamping berdasarkan data petrografi padi Formasi Sentolo di sepanjang lintasan Pengasih.E Miocene Rajamandala Lst in Sanghyang section 180m thick.id/artikel/pdf/perkembangan-sedimentologi-batugamping. Yonezu. 4. 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Two deep submarine paleovolcanoes: Tegalrejo (basaltic) and Baturagung (mainly pyroclastic material)) Muller.Sc.Developing the largest carbonate oil field in SE Asia. p. Conv. (online at: http://jurnal. 1. rising ~3000' above surrounding carbonate platform. exposed to fresh water leaching to form high quality reservoir rock with average 26% porosity and 100 mD permeability in interior.ac. University of New South Wales. p. (2014). p.3-D modeling of the deep electrical conductivity of Merapi volcano (Central Java): integrating magnetotellurics. West Java. Feldspathic tuff and pumice tuff are crystal vitric tuffs with more feldspar. Jakarta.Sandstone composition of the turbidite series of the Middle to Late Miocene of Majalengka sub-basin. 265-271. Exhib.cm. NW Java Basin. Jawa Barat. B. Indonesia. O22. olivine. 15-23. 18p.esdm. Murwanto. 205-222. F.Developing a large carbonate buildup field.id/index. F. 4p..go. Assoc. & V. 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Reefal Limestone.The Pliocene Selorejo Formation and its hydrocarbon prospects in Cepu and surrounding areas. Proc. Musliki. Bandung. 55-66.bgl. covered by Lidah Fm clays.com Sept 2016 . 3.Possible hydrocarbon accumulation within Eocene coarse clastic reservoir in the Northeast Java Basin. S. (1996). Marls of Kalibeng.Palaeogeographic interpretation based on lithostratigraphic units and relative sea level changes during the Plio-Pleistocene period in the Northeast Java Basin. Musliki. Conv. Globigerina Lst. Offshore NE Java good quality basal clastics in KE6. S. S.A geological trip to Cepu area for non-geoscientist personnel. Assoc.size planktonic foraminifera.Kembang zones.php/dir/article_detail/717) (Randu Kuning gold-copper porphyry prospect in Wonogiri/ Selogiri property with sheeted Cu-Au bearing quartz veins.esdm.Y. p. p. Bogomiring fields) produced from this facies) Muthi. (Very basic write-up of NE Java basin geology) Bibliography of Indonesia Geology. S. Proc. Chiang Mai. Indon. Ngrayong Fm unconformably overlain by different Late Miocene. Assoc. (1994).9 Ma. Assoc. International Symposium on Neogene. Proc. sedimentary processes and hydrocarbon prospect in the Northeast Java basin.The effect of Middle Miocene tectonic phase to the paleogeography. S. 43-54. All structural closures probably drilled. T. (IAGI).Musliki.The effect of structural style to the hydrocarbon accumulation in the Northeast Java Basin. Int. Symposium Geology and Environment. Geol.Characteristics of alteration and mineralization at Randu Kuning. Proc. Thailand. Best reservoirs Globigerina Lst facies: high porosity. p. (1992).Miocene volcanic arc) Nachrowi. (Comparison of NE Java with S Sumatra and E Kalimantan suggests Eocene. (online at: www. & Y. 379. p. 23rd Ann.E. Bandung. I Gde Basten. & Suratman (1996). A. Late Pliocene carbonates interpreted as shallowing. 26th Ann. Indon. Northeast Pacific Area. ~2. (IAGI). composed of sand. October.upward sequence starting in Late Pliocene. 1. 22-35. (1990). Conv. 6. Jakarta. (Abstract only) Musliki. (M Miocene N11-N12 Ngrayong Fm sandstone main reservoir in NE Java. Conv.Wonogiri Project. 19th Ann. Conv. p. Mineralization in quartz veins in and adjacent to microdiorite intrusion tied to large eroded volcanic centre in N-migrating Oligocene. S. 29th Ann. Pagerungan 2. Petroleum Assoc.vangorselslist. Significant gas (Balun field) and oil (Lidah. p. Indon. Kalinges and Kanopu Formations in the Northeast Java basin. p. Proc. Musliki. (IAGI). 28th Ann. JS5-1 and some had hydrocarbons).A Late Pliocene shallowing upward carbonate sequence and its reservoir potential. Litaay (2013). 86-96. 1. Indon. p. Geol.. 1. 20th Ann. Field Trip Guidebook. 1.Pliocene formations. Geol.permeability. not sure why) Musliki. Metatu. 131-138.The development of stratigraphic interpretation and its implication to the success of hydrocarbon exploration in the Northeast Java Basin. (IAGI). 25th Ann. Clastics in exploration wells in NE Java generally poor reservoir quality and no hydrocarbons. Conv.W. Conv. Indon. Majalah Geologi Indonesia 28. (1991). (IAGI). Geol. 1. (Late Pliocene Klitik-Ngepung-Selorejo Fms carbonate facies widely distributed in NE Java. Geol. Main lithologies diorites and breccias.The Neogene Kalimu. Bandung. Kuti. supposedly reflecting end-M Miocene orogeny/ global sea level drop. Indon.go. (IPA). Geol. p. (IAGI). S. Proc. Proc. 1-51. p. 15-28. Assoc. (IPA). Sasoni. sedimentology and petrography of turbidite deposits (study of Kerek Formation and Banyak member in the Kedungjati area.vangorselslist.A. Kon. West Java. In: J. 295-315. Masters Thesis. Indonesia.C. 19th Ann. shows six thrusts and four anticlines and synclines. corresponding to areas of lesser Eocene-Oligocene subsidence) Bibliography of Indonesia Geology. Petroleum Systems of SE Asia and Australasia. on NE-SW basement highs. Proc. H.. Nederl.V.A. p. H. Mitterer & J.Geological field mapping: to identify a structural pattern in Talagadatar as a thrust fold belt based on surface data and tectonic setting into Sumedang.M.Tertiary basin initiation and sedimentation. continuing into Kujung time (OligoceneMiocene).A. AAPG 2007 Ann. 1-250. p. Heavy oils (API <22°) are biodegraded in shallow reservoirs. Indonesia. Howes & R.C. (NW Java Basin on-and offshore oils mainly derived from Oligocene fluvial-deltaic Talangakar Fm. Isotope and biomarker data identified two oil families: (1) marine influenced delta front-prodelta settings and (2) from higher plant-rich delta plain.E. R. and (3) two oils with intermediate-high sulfur content suggestive of marine carbonate depositional setting. p. Napitupulu.Tertiary basin initiation and sedimentation. p. (IAGI). p. Mounded geometries of shallow-water carbonates. not tectonic or fault-initiated. Dragan & A. (2007). Ph. NE of Bandung. although high pristane/phytane. (1998).Organic geochemistry and thermal maturity modeling of hydrocarbon generation in the NW Java Basin. Rumende (2012). Geol.0 82 www. (Three source rock facies in NW Java Basin based on biomarker composition of oil: (1) deltaic withtypically high concentration of oleanane. Indon.H. Carroll (2007). H. J. Conv. Indon. 1. 149-174.Nahrowi. 2012-GD-11. Simo. A. Indon. Assoc. Prolific carbonate accumulations formed in areas with ~500 m or less Oligocene-M Miocene subsidence. L. etc. East Java Basin. p. Proc. Mild initial subsidence during Eocene increases with time) Naranjo. ('Aspects of stratigraphy.A. 339-361. Napitupulu. Major carbonate platform formed in N part of basin. Indonesia.E Pliocene and Late PlioceneE Pleistocene) Naizheng Du (1988). East Java Basin. Oligocene-Miocene isochron map shows change to WNW-ESE orientation. Madison. Noble (eds. (2) probably lacustrine with abundant botryococcane. etc. N. with API gravities 17°-53°. Assoc. 41st Ann. Post-generative alteration processes widespread..M. Ed. Proc. Conf.Post-generative alteration effects on petroleum in the onshore Northwest Java basin. Thesis University of Texas at Dallas. 31. inconsistent with rift origin for earlier basin history. Putra. may be mixed with oil from a non-carbonate source) Naranjo. & Suratman (1990). etc. (IAGI). Passive basin fill of initial Eocene-Oligocene Ngimbang Fm clastic-dominated sedimentation suggesst pronounced paleo-basement topography. Jakarta 1997.. conflict with this interpretation. Yogyakarta. p. 667-679.com Sept 2016 . but onshore part of basin appears to be constructed on pre-existing basement structural grain.D.C. Geol.V. 1-70. (Fieldwork in Sumedang area at Talagadatar. N.T. Late Miocene. 6. forming fold-thrust system with two periods of activity.delta front environment) Napitupulu. E. C Java') Naibaho. R.Differentiation of oils from the NW Java Basin into three oil types based on biomarker composition. sedimentologi dan petrografi endapan turbidit (studi kasus: Formasi Kerek & Anggota Banyak daerah Kedungjati. (Unpublished) (Majority of proposed E Java Basin formation mechanisms back-arc related. Two SW-trending projections from platform represent buildups formed on paleohighs.Aspek stratigrafi. Kristiono & I. Conv. Int.R. Organic Geochem.On some silicified woods from the Quaternary of Indonesia. Jawa Tengah). areas with greater subsidence (up to 900 m) became sediment-starved deeps. Mitterer (2000). Morelos-Garcia (1997). Subsidence rates increased at this time.A. University of Wisconsin. Akademie Wetenschappen B 91. Conv..Y. Ellis & R.) Proc.R. Petroleum Assoc. J. Pristane to phytane biomarker ratios severely affected by evaporative fractionation. Indonesia. (Abstract only) (Seismic isochron mapping shows axis of Eocene-Oligocene E Java basin trended NE-SW. J. 2. Petroleum Assoc. 6. ('The epithermal god deposit of Cirotan. Untung & Y. Latest deformation is N-S compression) Natori. 6. Proc. 81-89. intrusive in rhyolitic ignimbrites dated as 9. p. Res. Centre (GRDC). II.Enige voorlopige opmerkingen omtrent de hydrogeologie de Brantasvlakte. p. Thesis Sarjana. (Unpublished) ('Geology of coal deposits in the Cibobos-Cimandiri area.com Sept 2016 . (1993). W Java. high salinities. Abdullah & T.5 Ma.Foraminifera from Central Jawa. C. Dev.S. H. In: M. (Microtectonic analysis of NE-SW directed M Miocene syndepositional slump structures in deep-water deposits.H. ('Some preliminary remarks on the hydrogeology of the Brantas plain'. Sect. 89-101. 680-689. (IAGI). Proc 22nd Ann.W. P. (1978). Comptes Rendus Academie Sciences. 137146. Assoc. Marcoux (1992). Sato (eds. Dev. Bandung. and Exhib. SOT-11. Natori.. Mud volcanoes may have been active in area during Majapahit empire (see also Satyana 2008)) Natawidjaja.) Gravity and geological studies in Jawa. Jakarta 2006 Int.East Java Basins. Bandung.Japan Joint Research Program on Regional Tectonics of Southeast Asia. (1972).O.0 83 www. H.Paleomagnetic and geochronological constraints on the Cretaceous. Abdullah (2006). Indonesia. A.Correlation of the Tertiary lithostratigraphic units in the Java Sea and adjacent areas. (IPA). SW Java. 1-238. D.Magnetic properties of igneous rocks from Banyuwangi. 33-41. Geol. Bijaksana & C. A.Foraminifera from West Jawa. L. Bandung. Indonesia. (Extended Abstract) (Paleomagnetic study of area of ‘Old Andesites’ near Yogyakarta suggest paleolatitudes of C Java moved from 16-20°S in Cretaceous-Eocene (~76-47 Ma) to between 12-13°S in Oligocene (~30-25 Ma). Spec.-Indisch Natuurwetenschappelijk Congres.. Siregar & F.Japan Joint Research Program on Regional Tectonics of Southeast Asia. Sato (eds. Sudiyono. with correlation of stratigraphic successions) Nehlig. West Java') Nash. First Ann.Geological structures of Penosogan area Kebumen. G. post M Miocene extensional structures E of Karangsambung. Publ.A. Indonesia. p. P. Physics 16. Geol. 6.Le gisement d’or epithermal de Cirotan (Ouest Java. Jawa Barat. S. Indonesian J. (1931).Nas. Geosciences Conf. Centre (GRDC) Spec. Banten Selatan. Geologie-geografie. Conv. 10-11° S in Miocene (6-11 Ma). Nawawi. Publ. Ed. to 7°-8° S today. D. Proc. Indonesia. Res.. 11-30.Miocene tectonic evolution of Java. Hasibuan (1978).. Handelingen 6e Nederl. microthermometric constraints'. Mahrizal & C. Pertamina BPPKA.5 Ma). L. Liong (2005).M. 1. Paris 315. well S of present position) Bibliography of Indonesia Geology. Bijaksana. Indon. (Paleomagnetic investigation of two igneous intrusions (no absolute age known) in Gunung Nangkajajar at E tip of Java near Banyuwangi. S. Kadar. p. (1986).I. Conv. Nayoan.. Ser.I. 821-827. Microthermometric study of fluid inclusions from Cirotan epithermal gold deposit in Citotok Mining District.) Gravity and geological studies in Jawa. Paleolatitude of these intrusions was~30° S. supporting hypothesis that C and E parts of Java formed microcontinent that collided with Sundaland in Late Cretaceous-Eocene (but: collision should be younger if continued to move N after Eocene?.vangorselslist. M. p. p. 4 p. Absence of phase separation suggests minimal erosion of 410m since mineralization) Ngkoimani. South Banten. p. HvG)) Ngkoimani. suggest mineralization under rel. Indon. (Brief overview of principal basins of Java Sea from S Sumatra to N Madura/ Barito. p.O. East Java and their reliability for paleomagnetic study. Seven E-W trending anticlines in Brantas River flood plain/ delta in E Java. 1-107. & E. Institut Teknologi Bandung.Geologi endapan batubara daerah Cibobos-Cimandiri. Untung & Y. In: M. J. Mineralized fractures tied to Pliocene quartz-microdiorite (4. Geol.H. Jakarta. Indonesie): contraintes microthermometriques. Suseno & A. p. Central Java: the significance of slump structures and extensional faults. 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Onshore sub-basins Ciputat.Petroleum systems of Northwest Java. and (2) area of Kotaagung. Yani/N Seribu Trough and Asri systems.C. In: J. Dardji (1994). Hehuwat (1980). Noble (eds. deep water facies with slope channel sands and slumped Nummulites limestone blocks) Nishimura.A. R.Niethammer. Nugrahanto. Difference in strike of Java and Sumatra exceeds 20 °. Pasir Bungur. 3. where graben structure was observed and ignimbrite eruption occurred at 1 Ma. In: S. K. Sebuku and Krakatau).H. C Ardjuna. Indon. p.D. etc. SouthCentral Java. so rotation of Sumatra and opening of Strait Sunda might have started before 2 Ma) Nishimura. Mitteilungen 28. p.Fission-track ages of the tuffs of the Pucangan and Kabuh Formations and the tektite at Sangiran. J. G.A. Offshore petroleum systems S Ardjuna.H. A. Gravity anomalies in (1) N of Ujung Kulon. subduction started at 710 Ma. S.com Sept 2016 . Suparka (1992). p.Neotectonics of the Strait of Sunda. collected by Tobler in 1902. 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Samples from Kesongo and Crewek 'mud volcanoes' in Randublatung zone of NE Java basin with planktonic foraminifera of zones N18-19. are Pliocene mineralization hosted in OligoMiocene 'Old Andesite' volcanics.I.306°C. Ledok.I. (online at: https://gsmpubl. District Gedang Sari.. N14/N12 and N7-N9 and E Miocene large foraminifera. Barianto & M.Penentuan batuan sumber Gununglumpur di sekitar Purwodadi berdasarkan kandungan fosil foraminifera..I.com Sept 2016 . D. Geol.id/fosi/berita-sedimentologi) (Identification of 12 M Eocene (P11). Suwarna (1999). Interpreted as marine slope deposits) Novita. Mineral and Energy Resources of SE Asia (GEOSEA ’98). Teknik Geologi (UGM) 2. 1:100. Suwarti. Jurusan Teknik Geologi FT UGM.Asalmuda jadi batupasir vulkaniklastik Formasi Kebo-Butak daerah Mojosari dan Kalinampu. Ed.) Proc.A Mangga & D. T. J.or.. Barianto & M. Congress Geology. Klaten. Yogyakarta. Bayat.C. 70-81. Jawa (1508-6). Amin & N. 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Clays of Late Miocene Cinambo Fm S of Majalengka E of Bandung mainly Type III kerogen.Fasies turbidit Formasi Halang di daerah Ajibarang. ('Hydrocarbon source rock potential of the Cinambo Formation in the Majalengka area. 41st Ann. Petroleum Assoc.php/dir/article_detail/250) Bibliography of Indonesia Geology. W Java. 3. 37th Ann. I.Utilizing image log to generate fracture density map in the Pangkah Field. 6p. Geol. Carbonates in four facies (1) reef front to reef crest boundstone.id/index. 137-145. J. 2012-E-03. at W end of Kendeng zone.0 96 www. Possible source rock is shale below Pelang Fm) Pramumijoyo. A. Indonesia. Sutiyono (2010). Jawa Barat.id/publication/index. Dextral slip on SFS began during M Miocene and normal faulting prevailed in Sunda Strait since 5 Ma.esdm. Geochemical analysis shows nalkane high in C8-C15 and C25-C28. Hendrizan (2009). 1.vangorselslist. Geologi Indonesia 4. Conv. Fracture density decays quickly in about 200' from main faulting zone. 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Indon. is hydrocarbon generative center.Karakteristik batuan sumber (source rock) hidrokarbon pada Formasi Batuasih di daerah Sukabumi. prevailing fracture direction NE-SW) Pramono H. Fasies dan lingkungan batuan karbonat Formasi Parigi di daerah Palimanan. Proc. p. p. Kamtono. Central Java. Foraminifera believed to indicate Early Miocene age (but faunal list includes mixture of E Miocene (Te5. E Java'.S. Miogypsinoides) and M Miocene (Tf1-2.geotek. 39th Ann. S. Tmax 405-489°C. Tmax: 435-458°C and HI 47-163 mg HC/TOC.17 %. Indon. M. Proc.go. Depositional environment reef and associated facies. p. Proc. HvG) Bibliography of Indonesia Geology. 1-6. IAGI (Ikatan Ahli Geologi Indonesia). resin)) Praptisih. Siregar (2011). Bandung. (LIPI). Jawa Timur. Rambatan Fm up to 1. show minor oil and gas potential. In: Proc. p.S.Studi batuan induk pada sub cekungan Serayu Utara.S. including boundstones. S. etc. Cirebon. Siregar & Kamtono (2008).1. 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Conv.R.microcontinent. but no comercial hydrocarbons. Tuban area.Identifikasi perubahan terumbu terhadap fluktuasi muka laut Formasi Paciran daerah Tuban. 40th Ann. (2009). 27th Ann.. Facies study of Paciran Fm reefal limestone along N coast of NE Java shows 5 eustatic cycles. p. W. K.gas show. Indonesia. Late Oligocene.W..R. Two deformation phases prior to onset of ‘Old Andesite’ subduction-related volcanism: Cretaceous-Paleocene subduction-related and Late Eocene post subduction (collisonal?) deformation) Prasetyadi. geophysics and geochemistry.H. 37-49. P. F. 2. Conf. shallow and inadequate hydrocarbon kitchens. 1. Geological Congress. Petroleum Assoc. Indon.. p. 1-291. (IPA). Indon. each 25.12 indicate sea level drop. ('Coral biostratigraphy of the Rajamandala Formation'. offshore southeast Sumatra. (Unpublished) ('Reef stratigraphy of the Paciran Formation in the Tuban area’. E Java) Premonowati (2001).H. Proc. 1-14. 27p. (in Indonesian) Pratomo. I. (IAGI). 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Central Java. (Abstract only) (Karangsambung melange complex does not only include Cretaceous-Paleocene Luk Ulo Complex.Stratigrafi terumbu Formasi Paciran daerah Tuban. PITIAGI2009-189.Holocene) Premonowati (2005). 31-51.H. Wahid (2016). Geol. D. A. 17th Int.0 99 www.W. Indon.vangorselslist. C. Indon. (1990). Petroleum Assoc. p. Teknologi Bandung (ITB). p. sea level changes. Proc. Recent well post-mortem re-evaluation and remapping of kitchens modifies understanding of petroleum system. but also Eocene Larangan complex with M Eocene Asterocyclina-bearing limestone in melange) Prasetyanto. Indonesia.com Sept 2016 . Wintolo (1997). Volcanic gravity tectonics in Pleistocene considerable influence on petroleum play) Premonowati. Proc. I. E. Proc.Jatim.Tuban and Camar troughs (East Java basin) revival: new insight. Jakarta. Assoc. M. Conv. Jakarta. Plio-Pleistocene Paciran carbonate platform formed since 4 Ma (N19). Premonowati (1996). Proc. (Tuban and Camar Troughs in Offshore NE Java Basin surrounded by dry holes and generally condemned as lean. Geol. Rahayu. Age here shown as Late Miocene. D. Fukuoka. Jakarta. 37-47. (IAGI). Saputra. Jawa Barat. Geol.The implications of basin modeling for exploration. p. W Java) Premonowati (1998).daerah pantai utara Jawa Timur.E. Reef 1 deposited in Zone Bibliography of Indonesia Geology. Raseno. Geol.Biostratigrafi dan spesiesasi koral Formasi Rajamandala. Assoc. 25 th Ann. 17th Ann. (IAGI). Assoc. 4p.Understanding the petroleum system of North Serayu Basin: an integrated approach from geology. 21st Ann. Reefs 1. Many oil seeps and all elements of viable petroleum system.Geologi Formasi Paciran. F. IPA16-63-SG. Ed. Thesis Inst. Twelve reefal units.50 m thick. A. A. Indon.H. Ph. Oil shows present in Tuban-1 and other dry-holes may also have oil. Utomo. Proc. Y. B. Reef 2 at 5 Ma (Zone N19). p. ('Ecological stratification in the Holocene reef of Paciran Formation. Proc. 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Geol. to determine paleotemperature fluctuations and to validate sea level changes of Reef 1 to Reef 17 units from 4 Ma. Koesoemadinata. (Summary of Premonowati thesis work on Pleistocene Paciran limestone.P. After that drastic rise in paleotemperature) Premonowati. East Java. Proc.9 Ma. 57-74. Sulistiyana & D. 1. (Oxygen and carbon isotope analysis from Paciran limestone Fm to validate sea level changes during Reef 1Reef 12 formation between 4 Ma. Ed. Lamongan. Simposium Nas. Pacitan Region-East Java. Proc. Tectonic uplift caused Paciran Fm outcrops at 335m above sea level now) Premonowati. Prastistho & I. Early reef formtion (reef 1 to reef 3 between 4. Assoc. Harsono Pringgoprawiro & W. 2. 4.) Proc.0 100 www.iatmi. Modeled as transgressive-aggradational shallow marine sheet sands) Premonowati. R. Tuban area.Allostratigraphy of Punung paleoreef based on lithofacies distributions.pdf) (Semanggi field 1900 BPM discovery. Harsono Pringgoprawiro & W. 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Jurnal Teknologi Mineral (ITB) 12. Assoc. a case study from Tanjung Kodok.S. Makassar.P. (online at: www. Rahardjo. p. (IAGI). Hantoro (2005). p. Temperatures fluctuating until Reef 12 (E Holocene)) Premonowati..vangorselslist._UPNVY. Assoc. Pringgoprawiro & W. IATMI. p.4 Ma) stagnant temperature and almost warmer. based on terrace morphology. S. Harsono Pringgoprawiro & W.esdm. R. Sinulingga. Conv.bgl.Model of reef development in response to sea level fluctuation and isotope stratigraphy of Paciran Formation. Indonesia. Zulkarnain et al. Reef 1.P.1.Recent. Seminar on Nuclear Geology and Mining Resources.4 Ma) stagnant temperatures and almost warmer condition.Reef 8 (2.Stratigrafi isotop oksigen dan karbon dari Formasi Paciran Jawa Timur. (eds. TS01.P. Hantoro (1999).59 Ma)Reef 8 (1.or. Prastistho & I.S.) Premonowati. 208-219. (IAGI). (On M Miocene Punung Fm reefal limestone in S Mountains. B. W block more productive than E. Firdaus (2011). Not much detail) Premonowati.go. Hantoro (2000). (IAGI). Koesoemadinata. Firdaus (2012).7 Ma). 1 p. Mubandi. B. Conv.Prospectivity analysis of Java island for porphyry and epithermal deposits. p. p.Geochemistry of the Tertiary low potassium volcanics in East Java. (IAGI).The occurrence of plagiogranite in East Java. Joint Session 30th HAGI.Miocene carbonate mound of Gunung Maindu. Geoph.S.e. Indon. Mardani & V. East Java. Buletin Geologi (ITB) 37. (IAGI). Tuban: an analogue model for prospective carbonate mound hydrocarbon reservoirs in the East Java basin. 40 km N of Boyolali. Geol. Assoc.. Indonesia. A. E Java. 3p. Indon. Not much detail) Priyantoro. p. B. Wiyono (2005). showing N part of Seribu Mts uplifted higher than S part. A. 28th Ann. Multiple coarsening-upward packages.Premonowati & W.Genesa bentonit di kecamatan Wonosegoro Kabupaten Boyolalai. Selogiri in N and Wediombo at S coast.S. C Java. both hosted by old volcanics and intrusives. p.' Bentonite layer in turbiditic clastics series in W Kendeng Zone fold belt.Genesa deposit mangaan daerah Kliripan dan sekitarnya kecamatan kokap kabupaten Kulon Progo DIY. (Extended Abstract) Prihatmoko (1998). p. 30th Indon. 47-56. Geol.14th PERHAPI Ann.com Sept 2016 . Sukandarrumicli & S. PITIAGI2009-046. M. Surabaya. Proc. Semarang. represents regional influx of quartz sandstones in region. Assoc. NE Java. (Two as yet non-commercial mineralization/ alteration systems identified around C Java Southern Mountains... probably related to development of Quaternary magmatic arc to N) Priyanto.5 km deeper than high-sulfidation system of Wediombo. Assoc. Setyawan (1999). 11p. East Java basin. p. ('The genesis of bentonite at Wonosegoro district. Geol. (IAGI). Priangga Utama.Fasies and diagenesa batugamping Formasi Rajamandala. D. Jakarta.B. Geol. Assoc. Montong. Conv. Proc. (1997). 15-28. 1. (Abstract only) (M Miocene Ngrayong sandstone studied in 50m section at Prantakan River. i. 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W. with examples from C Java Southern Mountains’) Rahardjo. Yogyakarta. 77-87.27% .Reflektan vitrinite dan komposisi maseral seam batubara Eosen Formasi Nanggulan daerah Kalisonggo. Maha & A.Pliocene zonation of 7 pollen zones. with average vitrinite reflectance 0. Assoc. Geol.com Sept 2016 . calibrated to planktonic foram zonation) Rahardjo.Prelimanary result of foraminiferal biostratigraphy of Southern Mountains Tertiary rocks. Sediments soft and hardly diagenetically altered. (IAGI). Late Eocene coal of Nanggulan Fm deposited in telmatic to forest marsh environment. 135-140. Geol. E. Coal thickness 53 cm. ('Pollen zonation for the Tertiary of Java Island'. 1.. Res. Macerals comprise vitrinite texto-ulminite. (Lens-like geometries and overlying M Eocene turbiditic clastics suggest Nummulite-Assilina packstones in Bayat area are redeposited blocks in deeper water environment. Coal rank is lignite. Pre-Tertiary metamorphics with SW-NE trending foliation) Rahardjo. Geol. (On morphology and evolution of karst in Gunung Sewu/ Southern Mountains. p. & M. S. Rosidi (1977).B. 205-220. 20p. A. Conv. Geol.. (‘Problems of carbonate stratigraphy. (IAGI). 23rd Ann. Nanggulan Fm coal depositional facies is forest swamp) Rahmad.T.Paleoenvironment reconstruction of sedimentary sequence of the Baturagung escarpment. Revue Geomorphologie Dynamique 34. E flank of Kulon Progo Dome. Java. W of Yogya. Proc.Un karst en zone intertropicale: le Gunung Sewu a Java: aspects morphologiques et concepts evolutifs.. ('Vitrinite reflectance and maceral composition of Nanggulan Fm Eocene coal seam. 87-92. Kalisonggo area. (2002). Rahardjo. Seminar Potensi geologi Pegunungan Selatan dalam pengembangan wilayah. Yogyakarta Special Province. 6. Eocene. 30. Spec. M. HvG). Wartono (1983). Rodhi (2008).Geological map of the Yogyakarta Quadrangle. 39th Ann. Rahardjo. Assoc.M. Conv. Geol. Nugrahaningsi & E. (IAGI). 1. 1-16. Assoc. Res.Quinif. Proc. Syafri.Permasalahan pada stratigrafi batuan karbonat (dengan beberapa kasus contoh di Pegunungan Selatan Jawa Tengah). p. Dev. Geologi Indonesia (IAGI) 9. W. Daerah Istimewa Yogyakarta. Buletin Geologi (ITB) Spec.A. Central Java.37%. Bayat area. Kabupaten Kulon Progo. Geol. Geol. N. 6. (Brief review of Central Java geology) Ratman. G. Gunung Sewu. Haidar. Dev. A. Ranikothalia. Conv. Karyanto. B.F. p. (E Java zones of high overpressure in: (1) post-Tuban Fm. jalur engukuran Padasan. N.vangorselslist. E-M Miocene Kerk Fm sandstones poor reservoir quality (2-10% porosity). S. (4) E Miocene carbonates no longer develop upward. Hapsoro. Proc. Samodra (2004). 181-186.Djuwangi.Unravel Kendeng petroleum system enigma: recent update from transect surface observation of Kedungjati. Ratman. 2012-SS-05.The geology from Gunung Slamet to the Dieng Plateau. p.moderate-high overpressure. etc. Eocene Nummulites. & H. Seismic facies analysis showed 5 growth stages: (1) initial Rupelian carbonate aggradation. Arifin et al.M. (2) Tuban Fm. 37th Ann. in Wonosari and surrounding area'. In: Stratigrafi Pulau Jawa.R. 3 (147). ('Biostratigraphic study and carbonate microfacies analysis of the Wungkal Gamping Formation. Widada (2013). Y. but probably = Sukowati. D.Peta Geologi Indonesia Lembar Surabaya. HvG) in NE Java Basin is one of mature oil fields in Oligo-Miocene carbonates of Kujung Fm. Res. Bull. Indon. p. Budiman & I. and Kepek (Late Miocene-Pliocene. 1-12. Central Java'. N. Klaten. IPA15-G-065.) Ramadhan.Studi biostratigrafi dan analisis mikrofasies batugamping. Rahardjo (2012). C Java'.E Miocene backstepping carbonates.B: Oyo-Wonosari Fm probably older. 1.000. Onshore East Java Basin: impact of fluctuating relative sea-level change to facies development. Centre (GRDC). p. Jakarta. Discocyclina. Hutasoit. Formasi Wungkal Gamping.. Saputra. Assoc. (3) Late Oligocene. Jakarta. (2013). Petroleum Assoc. ('Rama Field' (not real name. 5p. M. Geol. (IPA). A. 1: 1. Bandung.low overpressure.Stratigrafi batuan Eosen di Perbukitan Jiwo. Purnamasari. Central Java. J. W. T. N.com Sept 2016 .C. C Java) Ramdhan. Bayat. Proc. L. Publ. Prasetyadi (2013)Organism variety effect on carbonate rock porosity of Jonggrangan Formation: alternative approach to predict porosity complexity. Hakim.D.Stratigrafi dan lingkungan lengendapan batuan karbonat.I. Bandung. p. (' Stratigraphy and depositional environment of carbonate rocks. (3) Kujung Fm carbonate buildups. M. IPA13-SG-056. Novian & W. F.Sadirsan. 39th Ann. 9p. Daniar. Robinson (1996). (5) E-M Miocene drowning of platform) Ramadhan. Premonowati Hadipramono & S. F. Geol. E. Pellatispira. Maha. HvG). 37 th Ann. but prograded towards basin.E. Gunung Gajah. E. Conv. Middle and Late Eocene limestones with Nummulites.. (IAGI). Ed. Proc. Wonosari (Late Miocene). Centre (GRDC). Sumber Daya Geologi 14. Fardiansyah (2015). IPA13-G-152. Majalah Geol. & G. East Java.Rahmawati. 1-34. Jawa Tengah. (Facies and porosity of E-M Miocene Jonggrangan Fm of Kulon Progo area. Gunung Sewi di daerah Wonosari dan sekitarnya. & H. Res. Yogyakarta. Cahyo & C. (2) major sea level drop followed by lowstand deposits in E Chattian. Spec. Tansinhokella.C. (IPA). M. Carbonates of Gunung Sewu three formations: Oyo (upper E Miocene-M Miocene). Dev.0 105 www. 41st Ann. Padasan Section. M. Assilina. Jakarta.. I. Goulty. Jawa Tengah.M. G.Assilina limestones and quartz sandstones on metamorphic basement. Res. Centre (GRDC).. N.hydrostatic pressure) Ratman. Operculina. (IPA). Samodra (1998). Alveolina. Dev. Indonesia 28.. Proc. 30. Petroleum Assoc. Bandung 20. p. Suwarti & H. ('Stratigraphy of Eocene rocks in the Jiwo Hills. 1-13. Bayat. Putra. M.A. Austrotrilina. Remaining potntial in 'Globigerina sands' in E and S parts of Kendeng zone near Ngawi) Ramadhan. grading upward into marls with Eocene (P13-P15) planktonics) Ratman. Conv. Indon.W.Kerek area.Importance of understanding geology in overpressure prediction: the example of the East Java Basin. 148-159.Seismic facies analysis of Oligo-Miocene reef in Rama Field. Petroleum Assoc. Bibliography of Indonesia Geology. Indon. 29-40. Indon. N.000. Conv. Gunung Gajah. Samodra (2004).. (Kendeng Zone depocenter in E Java and continuing into S Madura Basin with oil seeps and small oil-gas fields. Bibliography of Indonesia Geology. Conv. N-S orientation. Indon. 163-173. Dark grey breccious limestone with Nummulites below m1 breccia-layers. Indon. 3 days travel from Purbolingo. 6. Res. Jakarta. (1937). Jakarta. Fieldtrip guide book. Lowry (1996). (1930).Sandbox modeling of thrust-fold belt in Cimanintin area. Banjoemas.. p. Y. reticuspiralis) Reinhold. Bothropoma. (1930). burrowed sandstone with sharp upper-contact. 5-8 km long.9 Ma. between Bandung. Natuurkundig Tijdschrift Nederlandsch-Indie 90. (IPA). Petroleum Assoc.Cirebon. A. Abundance of gastropods Smaragdia. Upper Cibulakan Formation: its implications for reservoir distribution and prediction. Tijdschrift Nijverheid Landbouw in Nederlandsch-Indie 11. Conv. C Java) Reich. 1-29. Yogyakarta region’. & B. voorkomende op Java. Age suggested by associated zone Tf1 larger foram fauna ~ E Burdigalian. N. by Sr isotopes ~18. Offshore Northwest Java. Bittiinae points to seagrass environment.Raya. Indonesia). Y. T. gouv. Ed. Sandbody formed in response to sea-level lowstand. p.W. p. S C Java. 25th Ann. (‘On an occurrence of dacite on the S coast of Yogyakarta in the Gunung Sewu limestone area') Reitsema. Kusumanegara & P. Lowry (1999). Proc. S.. with Glossifungites surface and siderite mudclasts. Ser. Proc. W Java suggests 30-40% shortening) Reerink. p. Upper Cibulakan Formation. p. ARII ONWJ.W. 401-426.. between Nanggulan and Purworejo) Reksalegora.vangorselslist. 184 species. Kusumanegara & P. F. near villages Gegerbajing and Plana. Wesselingh & W. offshore Northwest Java.Cipamingkis River outcrop: a contribution to the understanding of "Main" reservoir geometry. from Middle Miocene and younger 'Globigerina Marls' and diatomites of C and E Java) Reitsema.Cipamingkis River field trip: a visit to an outcrop analog of the "Main" Interval. Lower bounding contact discordant with underlying interbedded sandstone and mudstone. siltstones and mudstones. West Java. 43-132. Indon. Sapiie (2003). 362-363. glauconitic sandstone. Sandbodies of same age and similar facies in W Java outcrops pinch out over 500 m. Four new gastropod species: Bothropoma mediocarinata. in het Goenoeng Sewoe kalksteengebied..Over een voorkomen van daciet aan de zuidkust van Jogjakarta. E. Annal. Laterally extensive and correlative over inter-field distances (10's of km). Serie 12. 25th Ann. 2. (Two sandbody types in "Main" interval: (1): sharp-based. p. Reksalegora. Rissoina banyungantiensis and R. (Study of E Miocene shallow marine mollusc fauna from Jonggrangan Fm near Banyunganti village. T. T. 259-266. in beds transgressive over 'Old Andesite' volcanics. Indon. 29th Ann. Geol. Hermanto. Djokjakarta. p. (‘An occurrence of Nummulites limestone at N edge of the ‘Western border mountains’.A depositional model for the “Main” interval. Proc. S.. Verhandelingen Geologisch-Mijnbouwkundig Genootschap Nederland Kol.A highly diverse molluscan seagrass fauna from the Late Burdigalian (Early Miocene) of Banjung Ante (South-Central Java. S.Een voorkomen van Nummulieten kalksteen aan den noordrand van het Westelijk grensgebergte. Kusumanagara & P. Renema (2014). 1. Petroleum Assoc. Naturhist. 1-2 km wide. J.0 106 www. (Very brief.R. Petroleum Assoc.L. (IPA). Museums Wien.com Sept 2016 . Banyumas Residency. Progo Mts. Jakarta. Lower contact burrowed. including 158 carnivorous and herbivorous gastropods. Y. (IAGI). p. bioturbated. (Modeling of Plio-Pleistocene WNE-ESE trending ‘Majalengka fold-thrust belt’.P. Assoc. Upper Cibulakan Formation. 371-383. 116. (1865). p.Nota omtrent eene rijke aardoliesoort. in Poerbolinggo. Conv. Sumedang. 291-293. Reksalegora. (IPA). S.. (2): middle to lower shoreface "cleaning upward". (First and most elaborate paper on marine fossil diatoms of Indonesia. Natuurkundig Tijdschrift Nederlandsch-Indie 90. Plesiotrochus hasibuani. involving steep M-L Miocene bathyal sediments in Sumedang area. Lowre (1996). early report on oil seep in stream near villages of Kalian Jattan and Segran. 5-129.Fossil diatoms of the Neogene of Java and their zonal distribution.L. Archaeogastropoda. and Parigi Fm carbonates. Indonesia: I.. Indon. p. IPA14‐G‐138. Upper Cibulakan (Zones 16. S. in Cilamaya. Conductive features: (1) strong 'ocean effect' at S-most site. 12). E. continuous sheet-like deposits and channel-levee features. Initial eruptions along NE-SW trend. Rembangian (M Miocene) assemblage 89 species. Only S of Purwakarta lower part of U Cibulakan Mb sufficiently mature to generate hydrocarbons. 6. (Vent distributions in Azerbaijan mud volcanoes used to propose what controls distribution of 169 vents at Lusi mud volcano. Soc. Stewart & M. 121-141.Structural controls on mud volcano vent distributions: examples from Azerbaijan and Lusi. Letters 25. Muller. 10p. each ending with hemipelagic deposition. In E Tuban Area Ngrayong Units II-III three cycles of turbidite deposition.pdf) ('On fossil corals from Java Island'. Seismic facies identified: mounded mass transport complexes..The Rembangian (Middle Miocene) mollusc-fauna of Java.A hydrocarbon generation analysis in Northwest Java Basin using Lopatin's method.it/pub/images/docs/contents/102-2/Robba.Pamanuka -Kandanghaur between 2000-2300m. Armia. p.repository. 52 are proposed as new. E. (NW Java Basin producing from Jatibarang Volcanics.at/pdf_frei_remote/MON_GEO_0032_0165-0185. Jakarta.. p. (2013). Sediment provenance from NW) Ritter. Petroleum Assoc. Geol. Main locality Gunung Sel in Tji-Lanang valley. Prasetyo (2014). Tingay (2011). (IPA). 14th Ann. Neogene fauna composed almost entirely of extinct species. 38th Ann. Echternacht (1999).Reminton. Hoffmann-Rothe. 168.vangorselslist. Strat. mainly Langhian Tawun Fm) and review of collections of Naturalis Biodiversity Center. Conv. Top oil window (TTI 15) in Randegan (E part NW Java Basin) at 1800-2000 m. p. Vienna.E. A.N Cilamaya areas mature in S. Megastomia regina. M. (2) zone of very high conductivity in C part of profile (volcanic or geothermal activity?). East Tuban Area. E. Exesilla. Jakarta.naturalis.H. In: Reise der Oesterreichischen Fregatte Novara um die Erde in den Jahren 1857.A magnetotelluric profile across Central Java. new taxa Ilanga rebjongensis. (online at: www. I. Gerold. (online at: www.com Sept 2016 . (online at: www. CO2 content believed from dissolving carbonates of Baturaja Fm formed after burial of Talang Akar sediments with high content of carbonaceous materials) Reuss. Theil 2. Indonesia. S. Davies. p. four formerly described (Leucotina speciosa. 1859. K. Geophysical Res. Byrdina & F. 15. Ed.Gantar and S-ward. (IPA). 4. E Java.Tertiary and Quaternary fossil pyramidelloidean gastropods of Indonesia. A. p.nl/document/479757) (Descriptions of pyramidelloidean gastropods collected from Rembang anticlinorium (NE Java.M. Scripta Geologica 144. J. TTI 16 only in Purwakarta-1 in Jatibarang volcanics. Leiden. Rongga District) Rifqi. (M Miocene quartz-rich Ngrayong Fm prolific hydrocarbon reservoir in E Java Basin (>155 MMBO produced from 17 fields). changing to eruptions that follow E-W trends.A. East Java. 14. Pranyoto (1985). 165-185. locally eroded during next turbidite deposition cycle. 18 species incl.Uber fossile Korallen der Insel Java. 1858. East Java Basin.P.Seismic facies analysis of turbidite complex in Ngrayong Formation. parallel to Watukosek fault.pdf) (Langhian archaeogastropods from Burdigalian. R. Three main units in Ngrayong Fm. A. Geol. A.rivistaitalianadipaleontologia. Indonesia. 1-191. Conv. A. 2. O. (3) conductor in N (active fault zone?)) Robba. Petroleum Assoc. Staatsdruckerei. M. 267-292. Indon. Proc. Rivista Italiana Paleont. Mahfi. Proc. A. & U. Talang Akar Fm and Baturaja Fm equivalents. (1996). Pareucbelus pannekoeki and Leptothyra laddi) Robba. indicating regressive and transgressive phase of depositional cycle.0 107 www. 102.. 1013-1030. Baturaja Fm mature in Purwakarta.Langhian Tawun Fm/ Rembang Beds in Sedan-Tuban area of Rembang anticlinorium. London. Most Neogene species endemic to Indonesian Archipelago) Roberts. Nurnusanto.landesmuseum. subparallel to regional fold axes) Bibliography of Indonesia Geology. Arsadi. 42654268. NE Java. (1867). C. Ethalia stefanoi. Fajar & A. 23. 17 species of Neogene corals collected by Von Hochstetter during Austrian Novara Expedition 1857-1859. Nugraha. Talang Akar in Gantar. (Magnetotelluric data at 8 sites along N30°E striking profile in C Java. most undescribed species.J. Setiabudi (2014). Strong low velocity anomaly zone between Cilacap and Banyumas. in upper part of Nanggulan Fm. 4.and S-wave velocity structure beneath Central Java. Cikidang.) Sundaland Resources. Petroleum Assoc. Kerta. labradorite.F. Mineralization ages Late Miocene. Rocks tectonically mixed as result of subduction. pillow basalt). Int.F. Sulaksana (2006). (Gastropoda. Java. Peridotites in small outcrops in N and C part of Gunung Badak. Resource Geology 52.East Java and East Java Sea. Econ. p. Ed. 3-6: Enclosures. Seraphidae) from the Middle Eocene mollusc assemblage of Nanggulan (Yogyakarta province.C.a petroleum systems evaluation. 3. (Unpublished) (Comprehensive overview of NE Java basin stratigraphy and petroleum geology. SW Java. p. vol. (W Java and S Sumatera split up by Sunda Strait. PT (2002). schist) and sediments (greywacke. Three groups of magmatic-volcanic events: Eocene-Early Miocene. & H.Pliocene. Indonesia). metamorphics (quartzite. S. 53. mostly of hyperstene. Kedondong) and 'high base metal' (Cirotan. Gabbros as dikes with porphyric textures.Cikidang hydrothermal gold deposit in Western Java. all ranging from basaltic andesite with acidic-intermediate intrusives. A. Indon. 6.Tomographic imaging of P. Dahlius (eds.The new species Terebellum olympiae n. plus 'high silver' (Way Linggo). In: I. Conv.F. Low velocity anomaly also in Kebumen. coinciding with extensional oceanic basin toward land.. Pillow basalt-spilitic lavas outcrop in N part. red clay. A. Low velocity anomaly at LawuMerapi zone.com Sept 2016 . S. (Listing of 44 mollusc species. Proc. (IPA). In: Proc. F.. M. With paleogeographic maps Eocene (Ngimbang) to Pliocene (GL marls)) Rohadi. Geosains dalam Pembangunan Ekonomi & Kesejahteraan Serantau. Bibliography of Indonesia Geology. p. from water well outcrop near Watumarah. polymict breccias).vangorselslist. 1: Text. Jakarta. Nummulites lst. p. Fardiansyah (2013). Multiclient Study. Widiyantoro.ac. Vols. p. Tomography Simulation 24. Indonesia: joint inversion of the MERAMEX and MCGA earthquake data. High velocity anomaly pattern beneath W part of C Java may represent subducted Indo-Australian plate) Rohmana. 5p. J. 109-128. Syafri..East Java and Java Sea basinal area. phyllite. Ojolali).Robertson Research-Pertamina (1986). Proc. Multi-client Study. 2: Appendices. (online at: http://resources. and all hosted in Mio-Pliocene magmatic-volcanic group) Rosana. (2001). Novadhani & I. Cikotok mines). Prihatmoko & T. 95 p. (Tomographic inversions from combined local and regional earthquake events. planktonic foram zones P13-P14) Rosana. Host rocks Miocene lapilli tuff and breccia) Rosana. Age late M Eocene. Padova.P. Gold in low-sulfidation quartz-adularia-sericite(-calcite) vein deposits. + figs.D. Matsueda (2002). Mardiana & N. S. (Unpublished) Robertson Utama Indonesia. 4 vols. black shale. one new. serpentinite. I. Langkawi 2006. Soc. Conv. IPA13-SG-031. Palembang. Mio-Pliocene and Quaternary. 1-9.Low-sulfidation epithermal Au mineralization in Western Java and Southern Sumatra. Ann. Low sulfidation epithermal vein systems grouped into 'low base metal' (Cibaliung. Wibowo. West Java. M. Basuki & A.Petrology of Pre-Tertiary melange complex of Gunung Badak. U. Merapi’s magma source comes from S of Merapi. p. Indonesia.Z.pdf) (Gunung Badak melange in Ciletuh Bay. Geol. in particular volcanic and magmatic events. GunungPongkor.0 108 www. PutihDoh. S. stratigraphy. 341-352. M. Nugraha & Masturyono (2013). 37th Ann.unpad. locally serpentinized. Indon. (MGEI). mainly bipyramidal volcanic quartz) Rolando. with ophiolite (peridotite. (M Miocene sandstones of Jaten Fm in C Java Southern Mountains quartz-rich.Quartz-rich sandy facies behind the Miocene volcanic activity in South East Java: insight from sandstone characteristics within Jaten Formation.sp. 4 km W of Nanggulan. probably reflecting large dome of sediment.id/unpadcontent/uploads/publikasi_dosen/1D%20Persidangan%20Geosience%20UKM%20-ITB. vol. 41-44. gabbro.. (Cikidang gold deposit discovered in 1991 in Bayah dome gold district (also Pongkor. overlain by E Tertiary Ciletuh Fm sediments. Dewi. Memorie Scienze Geol. R. but geologically similar. Sukabumi.. A. petroleum geochemistry and petroleum geology.. Ciletuh Region.M. Afd.F. Amsterdam.pdf) (Large amounts of annual sediment discharge in modern rivers suggest very high denudation rates on Java (around 0.id/bsc/article/view/8409/3916) ('Petrology of ophiolite rocks in the Sodongparat area.Tagogapu (=Rajamandala Limestone.unpad.Sukabumi. L.knaw. (1925).digitallibrary.dwc. M. Sammlungen Geol. File E43. Akademie Wetenschappen Amsterdam. Ikhram & N. and emplacement can be equated with "Cordilleran" ophiolite. 28. p. 221-230. Lok Ulo area. Pretertiary ophiolite in Ciletuh area. R. Geological Survey. (online at: www. C. 65-78. 597-608. 000. L. (‘Four cross-sections through the Tertiary marl zone between Surabaya and Ngawi’ (Kendeng zone)) Rutten.Studien uber Foraminiferen aus Ost-Asien.5-2. probably granitic Sundaland basement) Rosana. Sukabumi. Kunti islands. (1916).000. Res. 19 p. Verhandelingen Geologisch-Mijnbouwkundig Genootschap Nederland Kol. Jawa (Quadr. 1: 100. p. 838-848. (online at: http://jurnal. only rel. 149-152.vangorselslist. Kon. L. ('On the direction of Tertiary mountain building movements on Java'.knaw.13-43. W. (1918). 2. Rutten. p.T.R. limestone and polymict breccias in Manuk.. 9. Geol.R. Akademie Wetenschappen. schist and quartzite as fragments of polymict breccias in N flank of Gunung Badak. Bandung.Petrologi batuan ofiolit daerah Sodongparat. 7. K. associated with sedimentary-volcanic and metamorphic rocks. 1:10. Proc. 11096. L. p.The geology of the Serang quadrangle.Geological map of Nanggulan area. p.. L.dwc. Amsterdam.D. Nederl. young volcanics and Miocene sediments without volcanic content are found) Rutten. while basalt is Mid-Ocean Ridge Basalt (MORB). Dev. p.ac. Akademie Wetenschappen.repository. (UNPAD) 13. Some retrograde metamorphism) Rothpletz.H. Nederl. Zwei Fundstellen von Lepidocyclina aus Java.Phyllite. (1943). Geol. Serie 3 (Molengraaffvolume). Kon. K.M.On the rate of denudation in Java. E.Vier dwarsprofielen door de Tertiaire mergelzone tusschen Soerabaja en Ngawi. Bandung. 322-324. Ophiolite sequence incomplete.nl/DL/publications/PU00015144. assemblage of basalt.Studi nannoplankton pada Formasi Karangsambung dan Totogan di daerah Luk Ulo. Ardiansyah (2015). 191-203. Amsterdam.naturalis.com Sept 2016 . Kon. (1925). p. & A. (online at: www.pdf) Bibliography of Indonesia Geology. 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W Java limestone belt between Cibadak. Suwitodirdjo & Suharsono (1991). Nederl. Sukabumi'.nl/DL/publications/PU00012275. gabbro and ultramafics. Java') Rusmana. Akademie Wetenschappen. Sedimentary rocks composed of greywacke in Mandra island. ('Nannoplankton studies in the Karangsambung and Totogan formations. 2.'Old Andesites' and 'brecciated Miocene' to the East of Buitenzorg ( Java). (1918). (English version of paper above.G. 27th Ann.R. unlike observations of Van Es and Ziegler.8 ± 2. Purnomo. It is delineated by N-S bounding fault N of Cirebon. In: L.Geosynclinal subsidence versus glacially controlled movements in Java and Sumatra. Bachtiar (1999). 211-220. J. Geol.Penggunaan paleoheatflow dalam penentuan sejarah kematangan batuan induk. Cekungan Jawa Timur Utara. obvious North. Kadarusman.The status of the OO-Brebes fault system. and its implication to hydrocarbon exploration in the Eastern Part of North West Java Basin.directed folding in Kendeng zone. 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(Presence of oil and gas seeps in volcanic areas of Java show presence of active petroleum systems under volcanic covers. Volcanic quiescence across Java from 18. (2016). Deep seismic lines in East Java Sea and South Java forearc suggest possibility of Pre-Eocene section in Australia-derived microcontinent(s) (But: proven oil source rocks on Australian NW Shelf older than Cretaceous. and N-ward shift of Quaternary volcanic arc in C Java) Satyana. and N-ward shifting of Quaternary volcanic arc in C Java. A. Indon. Common oil and gas seeps in volcanic areas of Java show presence of active petroleum systems underneath volcanic cover. left-lateral and (2) NW-SE. Indon. 30p. (Geochemistry of Sepanjang oil in Eocene reservoir from Kangean area in Java Sea and general East Java oils suggest possible presence of marine Lower Cretaceous-sourced oil.H. (2009).vangorselslist. 4p.0 116 www.New insight on tectonic of Central Java. leftlateral. IPA15-G-105.. subsidence of N part of C Java and indentation of northern coastline. p. Conv. HvG) Bibliography of Indonesia Geology. 39th Ann. right-lateral PamanukanCilacap Fault.a “Terra Incognita” in petroleum exploration: new considerations on the tectonic evolution and petroleum implications. Geoph. A. Proc. Two sets of fault zones. Gadjah Mada University.The emergence of Pre-Cenozoic petroleum system in East Java Basin: constraints from new data and interpretation of tectonic reconstruction. (Two major Paleogene strike-slip faults with opposing trends and slips responsible for indentation of Java coastline: (1) SW-NE trending Muria-Kebumen Fault. and (2) NW-SE Pamanukan-Cilacap Fault. Indon. IPA07-G-085.Tuban. Proc.Central Java. (2014). (2006). based on low oleanane and sterane content. 31st Ann. Faults caused indentations of N and S coastlines.com Sept 2016 . right-lateral. Seismic imaging and reservoir quality issues) Satyana. (IPA). 6. A. uplift of Serayu Range and exposure of pre-Tertiary Luk Ulo melange complex. Jakarta. Baturaja and M Cibulakan formations and (2) South (Gunung Kidul. This hydrocarbon prospectivity of Java Island so far unexplored. (2015). disappearance of S Mountains in southern C Java due to subsidence.Subvolcanic hydrocarbon prospectivity of Java: opportunities and challenges.Subvolcanic hydrocarbon prospectivity of Java: opportunities and challenges. trending transversal to Java Island responsible for collapse of S Mountains in these areas) Satyana. Ed. (Extended Abstract) (C Java conspicuous indentation of coastlines compared to W and E Java. In: International Conference on Java’s Southern Mountains. 40th Ann.Banyumas. and geochemistry. (IPA).Disappearance of the Java’s Southern Mountains in Kebumen and Lumajang depressions: tectonic collapses and indentations by Java’s transverse major fault zones. Presence of two opposite regional strike-slip faults crossing each other in southern C Java has configured petroleum geology of C Java) Satyana. and subsided northern C Java) Satyana. A. 1-22. N Trend carbonates prolific petroleum reservoirs. 15p. deep seismic. but so far unexplored. subsidence of North C Java.Jampang. Conv. Abstract AAPG Int. Conf. IPA16-573-G. Majalengka-Banyumas area and N Serayu area. Conv. Focus areas for this target suggested here is at border between W Java. (Two ‘gaps’ in Java Southern Mountains: (1) Kebumen Depression in C Java and (2) Lumajang Depression in SE Java. Solo.12 Ma.H. (HAGI). N Trend carbonates in back-arc setting.H. Indonesia and its petroleum implications. Areas with prospectivity: Banten Block. 39th Ann. Proc. Reservoirs M Miocene Tawun to E Pliocene Mundu sands and carbonates) Satyana. Conv. and (2) Muriah.Satyana. With Ngrayong Fm paleogeography) Satyana. Conv. (Outcrop studies in Sumedang area suggest Bogor Basin also received sediments from N (e. C. across middle of Java.H. (Extended Abstract) (E Java basin basin rich in gas. Deepwater and Frontier Exploration in Asia and Australasia Symposium. Indon. Assoc.com Sept 2016 . A. Porong-BD platform). MDA. In: R. Indonesia: regional evaluation on opportunities and risks. (IPA). (Major E-W left-lateral wrench zone. & Asnidar (2008). Ed. Depressions formed by isostatic subsidence compensating for uplifted volcanic arcs located to S.g.. (IPA). Geol. Oil fields in E Java have reservoirs of Ngrayong sands considered as deepwater deposits on slope of Rembang Zone. A. 23 p. p. & M. A. Indon. natures and implications to petroleum system. (Brief but good overview of Oligo-Miocene carbonates distribution of East Java basin. East Java Basin: the origin and nature of a geologic border. Biogenic gases in two trends: (1) Surabaya. Conf. Indonesia: facies definition leading to recent significant discoveries. Yogyakarta. Jakarta. forming deformed zone 15-40 km wide and 675 km long from Rembang in W through Madura and Kangean Islands to Sakala offshore in E. West Java: opportunities for turbidite hydrocarbon play. E.vangorselslist.Oligo-Miocene carbonates of the East Java Basin. Biantoro & A. Bukit Tua. Proc. Geol. Petroleum Assoc. 20p. Indon. Proc. Fault Zone at hinge or shelf edge between stable E Sunda Shelf (Paternoster-Kangean micro-continent) in N and deep-water area with different basement lithology in S. 33 rd Ann.New observations on the evolution of the Bogor Basin. an axial depression with rapid deposition of Mio-Pleistocene sediments and subsequently compressed. Eocene clastics at Pagerunganand W Kangean) and (2) N Madura Platform (Kucung and Rancak carbonate reservoirs at KE.H. (Numerous mud diapirs and mud volcanoes in Bogor-North Serayu-Kendeng-Madura Strait Zone. North Serayu and Kendeng Zones. Abstract 65th EAGE Conf. Oil and gas seeps and producing oil and gas fields in same zone) Satyana. Jakarta.) Proc. Spec. Terang-Sirasun-Batur-Kubu).H. Syafri (2002). Bandung. 293-319. formed during Paleogene rifting. E. Spain. 34.H. Conv. Buletin Geologi( ITB). Barcelona. Oil seeps and oil fields in N Serayu Trough in turbiditic volcaniclastic sandstones. p. Indonesia. B. showing isolated platforms on WSW-ENE trending faulted basement highs.Madura Strait (Wunut. Armandita (2004).. 101116. 32nd Ann. Flower Bibliography of Indonesia Geology.Rembang-Madura-Kangean-Sakala (RMKS) Fault zone. Oyong. Ext. (Review of Mio-Pliocene deepwater sedimentation in Bogor.H.. In Plio-Pleistocene time trough/basins significantly uplifted and deformed. (IAGI). Darwis (2001). Maleo.0 117 www. abstract.A.Gas habitat of the East Java Basin. AAPG Int. (eds.Deepwater plays of Java. Prasetyadi (2004). 30th Ann. Djumlati (2003). Gases from Cepu High high-CO2 gas due to thermal degradation of carbonates. and currently form fold and thrust belts..Bawean (Kepodang Field). Eo-Oligocene Ngimbang carbonate at Suci. Jenggolo. (NE Java basin paper describing Oligo-Miocene deposition of carbonate buildups on ENE-WSW trending highs (W Cepu. Tectonic inversion started in mid-Miocene and peaked in Pleistocene time) Satyana. Raharjo & I. Petroleum Assoc. 5p. Erwanto & C. Deepwater plays viable in Java. p.. E Cepu. & A.Recent significant discoveries within Oligo-Miocene carbonates of the East Java Basin: integrating the petroleum geology. as suggested by Martodjojo (1984). followed by M Miocene and younger inversion) Satyana. Thermogenic gas in two trends: (1) Cepu. Vol.H. Stavanger 2003. Most sands deposited in ponded basins on slope area and as submarine fans on basin floor) Satyana.H. Proc. & Exhibition. & C.Kangean High (in Oligo-Miocene carbonates on Cepu High. Initiation of fault zone in late E Miocene in Sakala area. Indon. Noble et al. A. Congress. Fields in Pliocene-Pleistocene volcaniclastic turbidites of E Kendeng Zone also show prospectivity of deepwater plays in Java. A. formed during Eocene rifting. (IAGI) and GEOSEA 10th Reg. 4p. Luthfi (2003). IPA08-G-139. Armandita. 3.Mud diapirs and mud volcanoes in depressions of Java to Madura: origins. 6. 37-41. A. A. Payang). M Miocene in Rembang area. Assoc. upper M Miocene Cinambo. Lower Pliocene Subang and Bantarujeg Fms) not just from S.meets the future demand. R. p. P. & M. (IAGI) and 28th Ann. E.com Sept 2016 .Banyumas.B. Jakarta. deeply-rooted vertical master faults with upward diverging splays with reverse separations. 585-607. 2. 10. High CO2 gas (30-80%) in two areas: Cepu High. Conclusion disputed by Davies et al. p. (Shear wave velocity model of Jakarta Basin from seismic noise shows low-velocity basin under most of N Jakarta down to ~1-1. E.Bayah. Conv. & M. these splays are mapped as fold and fault belts trending W-E and WNW-ESE. 26. (IAGI).B. N Central Java.E.H. Most oils from terrestrial. Istadi & A.vangorselslist. Geol. Hawkins. Geol. & M. Indon. 1658-1675.H. Oyong. etc. (Study suggesting LUSI mud volcano is naturally occurring mud volcano in area prone to mud volcanism. Tectonic inversion observed. including Cepu-Surabaya-Madura.The LUSI mud volcano triggering controversy: was it caused by drilling? Marine Petroleum Geol. (Java Late Oligocene-Early Miocene widespread platform and reefal carbonates.L. Widiyantoro & B.E.M. 204. B.M. E. Masturyono. Murjaya. 68-102. Sutriono. 6. S. 55-66. N. 9. Assoc. Darmoyo (2010)-Was LUSI caused by drilling?. M.Geochemistry of the East Java Basin: new observations on oil grouping.structures on seismic sections.H. p. 1766-1784. 29th Ann. Ed. R. Shale diapirism common S of fault zone in thick shale sequences deposited rapidly to S of RMKS FZ) Satyana. J. p. Poleng. (2010) and Tingay (2009. Proc.M. Sutriono. Lower Kujung and Lower Tuban shales sources of oils and thermogenic gases. 918-931. Maleo (Madura straits). In: Proc. Volcanic quiescence in Java from 18-12 Ma (M Miocene) resulted in significant reefal carbonates development along S Mountains of Java. No volcanic material found in these carbonates. genetic gas types and trends of hydrocarbon habitats. IAGI Central Java section. Conf. Istadi & A. Irsyam. (Reply to Davies et al. In map view.Jampang. p. Proc. with Gunung Kidul. R. (2010) discussion. Marine Petroleum Geol. Karangbolong/Kalipucang in Banyumas.N. S Trend in intra-arc setting. 1. 27. Kepodang (Java sea) Wonolelo seep in W Cepu. Ngimbang.Lekukan struktur Jawa Tengah: suatu segmentasi sesar mendatar. Jakarta. showing basement-involved. who argued LUSI mud volcano was triggered by drilling) Saygin. and Bojonglopang in Jampang areas) Sawolo. & M. with transdimensional inversion of seismic noise. N Trend developed in back-arc setting. Indon Petrol. Sumberdaya geologi daerah istimewa Yogyakarta dan Jawa Tengah. Int.5 km) Bibliography of Indonesia Geology. Offshore oils more terrestrial than onshore.E. (Geochemical data from ~100 wells and seeps. Two trends: (1) N Trend. 32nd Ann. Rajamandala reefs developed prior to E Miocene Jampang volcanism. Extensional component of wrench zone subsided Paleogene rifted blocks like Central Deep and formed normal faults. Assoc.P..P. Jonggrangan in Kulon Progo. A. B. Kidul-Banyumas-Jampang areas. p. HAGI. Two wrench zones representing Paleogene tectonic elements of major shears in W Indonesia (NE-SW Sumatran Trend and SW-NE Meratus Trend) meet in C Java) Satyana. A. 31st Ann.M. Period also noted for 'Old Andesite' volcanism along S part of Java. Kennett (2016). Conv. Proc. 75-150 km away from Oligo-Miocene volcanic arc in S Java.H. Purwaningsih (2003). 2016)) Sawolo. M Cibulakan and Baturaja and (2) S Trend. Geophysical J. Biogenic gas in M Miocene-Pliocene reservoirs in Terang-Sirasun. and Ciputat-Jatibarang areas consists of carbonates of Kujung. Purwaningsih (2002). A.Lidah shales. Pandhu. (Similar to 2002 paper. Indonesia. Darmoyo (2009). Tuban. High CO2 associated with thermal degradation of Paleogene Kujung carbonates) Satyana. Purwaningsih (2003).. Prupuh. 27p. A.0 118 www.marginal marine facies. Conv.Authors reply to discussion.Geochemistry and habitats of oil and gas in the East Java Basin regional evaluation and new observations.Oligo-Miocene carbonates of Java: tectonic setting and effects of volcanism. Yogyakarta. (Indentation of C Java structure by wrench faults.SukabumiRajamandala areas. like Wonosari/Punung in Gunung Kidul. A.. Cummins.E. Purwaningsih (2002). Biogenic gases from Neogene Tawun.Imaging architecture of the Jakarta Basin. Conv. N. offshore Java Sea) Satyana. Cipta. No reefal carbonates in G. Indon. (IPA). Assoc. A.M. Conv. E Pliocene drift facies widespread from E-most-C Java to Bali Sea. & T. 189-212.. De Ingenieur in Nederlandsch-Indie (IV). F. gouvernement Jogjakarta. D. 4.A.A. Descriptions of cowrie shells from Miocene of Lodan anticline. 5th Ann. p. Two types: foram sand "drifts" deposited by bottom currents and foram "turbidites" deposited as submarine channel-fills and fans. composed almost entirely of volcaniclastic sediments. HvG)) Scheidecker.A. & D. p. (1937). (IPA). Geol.The marine mollusca of the Kendeng beds (East Java). 95-114. 6. W. p. Two lithofacies: (1) composed of mostly quartz (58-84%) and variety of lithic fragments. Petroleum Assoc. Mesozoic granitic continental crust and Late Cretaceous subduction complex areas to N interpreted to have supplied majority of quartz and lithic fragments. Similar globigerinid-rich facies in Late Pliocene Selorejo Fm of C and E Java.sp. (2) less pervasive volcanic facies. Petroleum Assoc.A. D. F.. (1939). J. Yogyakarta area'.The reservoir potential of Globigerinid sands in Indonesia. with undulose extinction (= metamorphic quartz?.naturalis. etc.com Sept 2016 . Jakarta.253/cgi-bin/ ) ('An occurrence of quartz sandstone. 23rd Ann. interpreted as sand-dominated submarine fan complex. Leidsche Geol. & C. Gastropoda). Prasetyo (1991). Proc.R. Seubert. Garrard & L. Quartz described as polycrystalline. (IPA). Drooger (1974).. ('Neogene Cypraeacea from East Java'. Musliki & M.W. (online at: www.M. p. p.L Eocene Ciletuh Fm f-vc sandstones and sandy conglomerates. 494-500.L. p. 20th Ann.Eocene submarine fan sedimentation in Southwest Java. Palaont. Ed. Natuurkundig Tijdschrift Nederlandsch-Indie 91. Volva surajensis n. and Amphiperaidae). daciet en contactmetamorphe gesteenten in het heuvelterrein nabij Godean. Facies development related to tectonic event. 1. 81.vangorselslist. R. (IPA). Gastropods) Schilder. Proc. dacite and contact metamorphic rocks in small hills near Godean. 11.28. Locality of G. Pliocene of Solo River and E Pleistocene of Mojokerto region. 195-210. Reitsema (1931). Petroleum Assoc. Late Pliocene examples appear restricted to Rembang Zone of NE Java) Schipper. Foram drift deposits in E JavaMadura Strait mostly latest Early Pliocene.Miogypsinidae from East Java and Madura. Neues Jahrbuch Mineral. Indon. B. NW of Godean. 1-14. collected during mapping by Bandung Geological survey) Schilder.) Schiller. while possible Eocene local volcanic arc is believed to have sourced volcanics. Schiller. (Second offshore oil discovery in Indonesia.8 Ma global sea level lowstand. F. "Foram drift" facies more common and best reservoir characteristics. B77. Cypraeidae. Part 3 (Families Eratoidae. S. Bibliography of Indonesia Geology. Gastropods from Upper Kalibeng and Pucangan Fms includes Zoila kendengensis. Jakarta. Proc.Scheibener. possibly Eocene sandstone with intrusive younger andesitic volcanics.nl/document/549360) (Part of series of papers on Kendeng Beds marine molluscs by Van Regteren Altena 1938-1950 and Schilder. partly coinciding with 3. W of Yogya.0 119 www. 196-202. Nederl. Indon.Java (Mollusca.repository. p. Pare. 3.Arjuna B structure: a case history. Upper Cibulakan Fm and 'Main' and 'Massive' sand reservoirs improve in quality away from crest of structure) Schilder.41. in 1968.Up to 30-45% primary porosity. 1. 100-1000 md perm and 30-40 m thick. Amsterdam. Mededelingen 12.W. Gastropoda. Akademie Wetenschappen. 1.Een voorkomen van kwartszandsteen. Taiclet (1976).Uber einige fossile Cypraeacea aus dem Sunda-Archipel. (Outcrops of M. Conv.. (online at: http://62. Reservoir quality of quartzose sst poor due to compaction and carbonate cementation). Conv. Jakarta. 1. p. (1941). ('On some fossil Cypraea from the Sunda Archipelago'. Indon. 171-194. (Porous limestones composed of sand-sized planktonic forams in outcrops and wells with variable reservoir quality and thickness. E. Proc. 2. 125-181. Kon.Neogene Cypraeacea aus Ost. Abdullah (1994). Wissensch. (1900). probably Pliocene-age shallow marine mollusc fauna) Schuppli. Zeitschrift 36. 216-217. long-lived M. Reichs-Museums Leiden ser. Abhandl. (online at: http://bhl. 5.Note sur deux especes de Lepidocyclina des Indes Neerlandaises. 11/111/15. ('Brief report on the geological situation of the South Rembang hill country'. Same paper as above) Schweitzer. Engelmann. p 1-10. 6.A new family of brachyuran (Crustacea. 1-64. (Flenley 1979. R. Gaedicke. B. 1. Roeser. Geologische und palaontologische Ergebnisse der Trinil-Expedition (1907-1908). (1932). J. H. (1911).nl/cgi/t/text/get-pdf?c=scripta.L. C. Lepidocyclina insulae natalis (probably E Miocene Eulepidina. 6. with 21 species no longer present on Java. Lowland tropical species appear to be absent. 235-257. H. Walther (1962). At 80m above sea level karstified limestone overlain by thin conglomerates and sands with clasts of manganese impregnated limestone and wellpreserved. Ed. ('On a new occurrence of Pliocene on the Gunung Sadeng near Puger (E Java)'. antillea (Gr. Paleontol. H. Decapoda. Java) and its significance for the age of the manganese mineralization’) Schmid. Reichert. p. are E Miocene Old Andesites overlain by M Miocene marls and Wonosari reefal limestones. Verhandelingen 3. & H. 128-134.repository. E Java. (online at: www. In: M. Van Zeist 1984: presence of leaves with entire margins and drip-tips suggest everwet conditions. Djajadihardja & A. Bonadio (2009). HvG) from Ngembak well. often at altitudes of 700-1500m. Bayerischen Akad. and stellate Lepidocyclina martini from Miocene of Madura. & H. p.) Die Pithecanthropus-Schichten auf Java. (‘The flora of the Trinil Beds’. cushmani (~N8?) and M.U. Y. 1. Leipzig. M. Meyer. Suppl. 25. Kl.. Goneplacoidea) from the Eocene of Java. C.Kort verslag over de geologische situatie van het Zuid-Rembangsche heuvelland. Walther (1962). 6. C. Transtensional pull-apart basins along W Sunda Strait. (‘A new Pliocene locality at Gunung Sadeng near Puger (E.M.(Three E-M Miocene miogypsinid species assemblages from same samples studied for lepidocyclinids and planktonics by Van der Vlerk and Postuma (1967): rel.Tectonic features of the southern Sumatra-Java forearc of Indonesia.A. F.) Schmid. Kon. Math. etc. p. p.SW Java: Paleogene inner wedge and Neogene.org.ala.com Sept 2016 . 1. Tectonics 21. (Seismic suggests two units in accretionary wedge off SW Sumatra. Sammlungen Geol. SE Java. globulina (N5-N7?). Prex (2002). but known from other parts of SE Asia.au/bibliography/7643/summary) ('Monograph of the fossil flora of the Pithecanthropus beds'.E.Recent outer wedge. Jaarboek Mijnwezen Nederlandsch-Indie 59 (1930).naturalis. With analyses of foraminifera and molluscs by Van der Vlerk and Martin) Schuster. (1911). collected by Verbeek) Schluter. not monsoonal with pronounced dry season like C-E Java today)) Schuster. N9)) Schlumberger.nl/document/552395) ('Note on two species of Lepidocyclina from the Netherlands Indies'.Uber ein neues Pliozan-Vorkommen auf dem Gunung Sadeng bei Puger (Ost-Java). Central Java Pleistocene plant fossils from Trinil area 52 species.. Feldmann & C.Monographie der fossilen Flora der Pithecanthropus-Schichten.W.idno=09138a01) Bibliography of Indonesia Geology.vangorselslist. Indonesia. H. C. p. Blanckenhorn (eds. p.scriptageologica. Scripta Geologica 138. Schreckenberger. Geol. peripheroronda zone.Ein neuer Fundpunkt von Pliozan auf dem Gunung Sadeng bei Puger (OstJava) und seine Bedeutung fur das Alter der Manganvererzung. 95-121. Pliocene in S Mountains of SE Java N of Puger village. All suggesting climate cooler than today (possibly ~6-7°C less)). Munchen. 247-276. J. locally with metasomatic manganese mineralization. Jahrbuch 80.-phys. Selenka & M.W. F. p. Early report on Mio-Pleistocene stratigraphy and structure of Kendeng zone by BPM geologist. (online at: www.Die Flora der Trinil-Schichten.0 120 www. Proc. Derewetzky. Jakarta. Indon. daerah lama. Int. 2nd Ann. Proc. Makassar. Conv. Two Tethyan molluscs species recorded for first time from Nanggulan. (2011). Indonesia. Wikanswasti & A. IPA14-G-309.M. Priambodo.E Miocene subsurface carbonate buildups and associated deeper water calciturbidites and debrites similar range of environments as outcrops of Late Oligocene Rajamandala Lst) Sembodo (1973). Proc.) Proc. Bellier (1993). Maryanto.Geosciences. East Java Basin testing 488 and 744 BOPD from DST in M Miocene reefal limestone in July 2012. Petroleum Assoc. 5. B. p. R. Growth of Mid Miocene reefal limestone in area related to Miocene uplift event in area of earlier deep marine facies) Sebrier.Middle Miocene reefal limestone as a new exploration play in Ngimbang sub basin. Conv. Petroleum Assoc. C Java.E Pleistocene Citalang Fm of N Sumedang ~1000 m of fluvial deposits..Facies analysis and sequence stratigraphy of Tertiary subsurface (Cepu Block) and surface (Rajamandala Limestone) carbonates of Java.Miocene to Recent kinematic evolution around the Sunda Strait and southern end of the great Sumatra Fault: microtectonic approach. IPA15-G-039.I. 37-40. 403-414. F. p. an overlooked reservoir. East Java. IPA11-G-063. play types and play fairway and underexplored play in East Java Basin. Rieb (eds. (Extended Abstract) (P-1 Well. D. JCM2011-097. 45-48. D. 36th HAGI and 40th IAGI Ann.structural framework. 6. In: B. Chiang Mai.osaka-cu. T.. Indonesia.a case study. Looks like typical Tethyan fauna) Scolari. (Review of geology and Cenozoic hydrocarbon plays in offshore E Java Basin in and around Pangkah PSC) Setiawan. French Indonesian Cooperation in Oceanography. Strohmenger. Ratanasthien & S. D.pdf) (Pliocene. a discussion on shared taxa. A. Jakarta. Osaka City University. ('New play. 5p. Conv. Tu P 12. Nugroho (2011). one of thickest non-marine deposits on Java.J. 38th Ann. In: EAGE 6th Int. 9p. S. perspektif baru: identifikasi batugamping N11-N14 pada sub cekungan Ngimbang menggunakan data seismik 2D. Jakarta. Nanggulan. Hakiki. 16p. M. Indon. Ardana Darma (2014). and Exhibition. p. (New gastropod species from M Eocene lower Nanggulan Fm('Axinea Beds')) Sebayang. C. p. Geosciences. Petroleum Assoc. D. p. 10th Ann. Ed. D. Sekti. Conv. p.J.D. R.ac. Jakarta. R. M.vangorselslist. old area. Facies map was also made to give a picture of the N11-N14 paleogeography. Proc.Middle Eocene molluscs from the eastern and western Tethys. Indon.Fluvial facies of the Citalang Formation (Pliocene-Early Pleistocene). Overall environment interpreted as braided streams) Setiawan. F. 1-15. Fullmer.com Sept 2016 . 30 Km NW of Ngimbang Sub Basin.Stratigraphic.The new species Sundabittium shutoi from the Middle Eocene of Nanggulan (Java.N. (IPA). (online at: http://dlisv03. Setiadi. (2001). S. C.Play baru. Java) Scolari. 53. Simo. Seismic shows presence of reefal limestone reflection patterns at M Miocene (N11-N14) level. Petroleum Assoc. Noeradi (2014).(New family to accommodate fossil crab Martinocarcinus ickeae Boehm 1922 from Late Eocene of Kali Puru.N. A. Padova. Bibliography of Indonesia Geology. possible equivalents of Bulu Limestone and limestones in Tapen 1 well between 1475-1760m) Sebayang. Saint Petersburg. (1999)..Tuban Sandstone. Conf.. Memorie Scienze Geol.Notes on formation evaluation in the Jatibarang volcanic reservoir. 35th Ann. Sapiie & D. Indonesia. Interpretation of M Miocene reefal buildups on 2D seismic in E Java basin. (IPA). (Cepu Block late M Eocene. Prasetyo & D. Pramumijoyo & O. K. (Eocene fossil molluscs from Nanggulan. Juliansyah & I. (2001). E of Cepu block. Indonesia).W. on Shallow Tethys (ST).P. Proc.L. J.media. West Java. (IPA). F. Joint.jp/infolib/user_contents/kiyo/DB00010811.. new perspective: identification of N11-N14 limestone in the Ngimbang sub-basin from 2D seismic data'. 12p. F. Twelve facies defined in four sections. Symp. Wardhana (2015). 189-199.. (IPA). 39th Ann. Jakarta. 44. Conv.I. Indon. 131-147.0 121 www. Deposition begins in E Eocene (P8) to M Eocene (P13). Conv. Prasetyadi (2013). Jakarta.com Sept 2016 . Provinsi Jawa Tengah. L.O. Epidote-glaucophane schist mainly glaucophane. 6. followed by suspension currents. epidote. Yogyakarta 2013.B. Southern Mountains. 6th Seminar Nasional Kebumian. Low quartz. Kecamatan Bayat.The genesis of Tertiary "Dakah Volcanic" in Karangsambung. 39th Ann.Future exploration play concept in Western Kendeng fold thrust belt: based on comprehensive stratigraphic and geochemical analyses of outcropped Miocene Kerek and Pelang Formation and oil seeps.I.Characteristic of turbidite deposits of Halang Formation based on outcrops and thin Section petrography description in Cisanggarung River. Kabupaten Klaten. Backarc magmatism after detachment of subducted slab between 270-500 km depth.E Miocene Kujung Fm carbonate reservoirs. Sunda Arc. Presence of blueschist facies confirms Jiwo Hills is one of high-P metamorphic terranes together with Luk Ulo (C Java). Several carbonate sedimentary rocks converted to garnet-wollastonite skarn under contact metamorphism caused by diabase intrusion. 105-121. (2015). Proc. IPA15-SG-094. Japan. avoiding partial slab melting. Deeper mantle is upwelling through this slab window and produce backarc magmas characterized by low 87Sr/86Sr and 143Nd/144Nd values (mantle array). Kebumen. mica schist. Bayat District.D. More than 90% of metallic mineral deposits located within Tertiary volcanic arc centers) Bibliography of Indonesia Geology.E Pliocene Halang Fm upper bathyal turbidites along Cisanggarung River. 11-23.S.. Arcs experienced CCW rotation during Cenozoic with W-most Java as rotational pole. H. calc-silicate schist. W Java subducted oceanic crust is old (Cretaceous) and cold. Erosional unconformity between E Eocene (P8) and M Eocene (P10). Lower part of Wungkal-Gamping Fm is debris flow.0 122 www. Petroleum Assoc. Serpentinites might have facilitated exhumation of blueschist in Jiwo Hills) Setiawan. Backarc magmatism since latest MioceneRecent in C and E Java.I. 35th Ann.Geoinformation of island arc magmatism and associated earth resources: a case study of Java Island.. marl and claystone. then shallowing until P13) Setijadji. Paleocurrent direction from N 280°-300°E (or SW?)) Setiawan. Sucipta (2011).. JCM2011105. resulting in adakitic igneous rocks. In: Proc. Well-defined volcanic belts since Oligocene. Central Java. p. L. phengite. (2005).ac. (2011). and hematite. Conv.140107-nugroho. conglomerate. D.E Oligocene island arc tholeiite volcanism in melange sediments of Karangsambung and Totogan Fm) Setiawati. N.(In offshore NE Java basin E Miocene Tuban Fm shale usually seal for Oligocene. Meratus (S Kalimantan). (IPA). Fukuoka. Formation comprises tuffaceous sandstone. Rare epidote-glaucophane schist crop out near exposure of serpentinite in W part of complex. (Descriptions of outcrops and thin sections of M Miocene. N. Jakarta. IPA11-SG-005. 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M. p.Sedimentology of Wonosari carbonates Southern Yogyakarta: outcrop study and petroleum implications. T. Min. (E Miocene Jampang Fm oldest volcanogenic deposit on Java.Middle and Late Pleistocene lavas at Sunda (0.W. & S.0. West Java. (2004). Setiawan et al. p. (IPA). Ed. Indonesia: an inferred timetable resolving the evolutionary history of the upper mantle.. Jakarta 2001. Gold in epithermal.G. (online at: https://www. Early Tertiary coal and shales likely source rocks. Adhiperdana. IPA08-G-083. West Java. 103-128. E. E.0. p. (Abstract only) (Datung of ~4-1 Ma old volcanic rocks around Bandung using radiometric ages and magnetic polarity) Sunardi. Kumai (2001).vangorselslist. Publ. Geochemical results from 200-400 m well samples of Paleogene sediments indicate mature and oil/gas prone source rocks. 2n FOSI Reg.18-0. Jakarta. Satyana (2006). deepening to N. Suharto (1989). E. Sudarmawan & A.jst.com Sept 2016 . Depositional environments from shallow S to deep N: (1) back reef-shelf with patch reef and algal foram packstones.jstage. W Java. 6.) Proc.3-2. p. Sudirman & T. Potential for significant petroleum accumulations appears greatest in E part) Sunardi. Conv. Survey Japan. Pliocene lavas dated by K-Ar as 4. Gondwana Res 4. p. Spec. 3. Bayah Dome. 107-111. Conf. lithic tuff. B.Stratigraphy review of Kuningan area in relation to the petroleum potential.H. Kosasih (1992). Nurdrajat. Base Tertiary ranges from >2000 meters depth to PreTertiary exposure at Ciletuh. N. and Geol. J. In: Epithermal gold in Asia and the Pacific. Hyodo & H. E. (2) reef zone with boundstones and Bibliography of Indonesia Geology. SW Java. Muchsin. (UNPAD) 9. & J. S. Breccias clasts mainly basalt.1. E.6 Ma. poorly known.S. Sedimentologists Forum.04 Ma) volcanoes) Sunarya. Amir. Kunto & R. Economic Geology 93. Bull.1 Ma and 3.. In: Stratigrafi Pulau Jawa. West Java. (S mountains of W Java largely consists of inverted sub-basins. Mineral Concentrations and Hydrocarbon Accumulations in the ESCAP Region series.. D.Facies analysis of the Cisubuh Formation outcrops analogues at Brebes-Tegal-Pemalang District. Central Java.unpad. AAPG Int. also skeletal limestone.. p. Resources Div.5.Magnetic polarity stratigraphy of the Plio-Pleistocene volcanic rocks in and around the Bandung Basin. Y.ac.pdf) (Kuningan area of Bogor Trough. Seminar.8 Ma at W and SW side of Bandung Basin.. UN ESCAP. Deep-Water Sedimentation of Southeast Asia. Indonesia. Resurgence in melting with 'Old Quaternary' lavas between ~1. ripped-up tuffaceous sandstone) Sunardi. E. ESCAP.id/wp-content/uploads/2012/07/2-Edy-Sunardi-STRATIGRAPHY-REVIEWOF-KUNINGAN-AREA.The epithermal gold deposits in the Cikotok area. simultaneous with uplift of Sunda Arc. Kimura (1998). Petroleum Assoc. Indonesia. shallow oil wells of Indonesia were drilled on oil seeps near Maja in N part of area by Reerink in 1871. Indon. (Abstract only) (Wonosari reefal carbonates rimmed shelf platform. E of Bandung and S of Cirebon. (Gold mined since 1936 Cikotok area. Dev.0 141 www. 43-47.Sunardi.jp/article/ganko/93/4/93_4_103/_pdf) (Bandung Basin underlain by late Cenozic volcanics. 30. sulpide-bearing quartz veins. 12p. West Java. Perth 2006. First. (Extended Abstract) Sunardi. (online at: http://ftgeologi.G. Hosted by propylitized Oligo-Miocene 'Old Andesites') Sunjaya. Tsukuba 1989. Indon. Stratigraphy and hydrocarbon plays of offshore NW Java Basin may extend to Kuningan area) Sunardi. & B. mainly in N-S trending fractures. 32nd Ann. 793. Petrol. In: First workshop on epithermal gold mineralization. Adhiperdana (2008). In: A. 125-138. 54-59. A. Y.The epithermal gold deposits in Cikotok area. with deformed Tertiary sediments and dissected arc remnants. Centre (GRDC). (eds. Scientific Contr.2 Ma) and Tangkuban Perahu (0. E. Sunarya.An account for the petroleum prospectivity in the Southern Mountains of west Java: a geological frontier in the west? Proc. Res.Lithofacies stratigraphy and characteristic of Jampang Formation. 6. (2011). Bandung. Geol.go. 4.S. packstones-grainstones cut by surge channels; (3) reef slope with packstones and rudstones; (4) toe to slope with planktonic packstones and wackestones. Diagenetic processes: micritization, dolomitization, and dissolution. Locally good porosities. M Miocene Sambipitu Fm may provide source rocks but distribution limited. Mio-Pliocene Kepek limestones and marls may partly seal Wonosari reefs. Oil seeps absent in area) Sunjaya E.S., M.I. Novian, E. Biantoro & A.H.Satyana (2006)- Exploration challenge on Kendeng zone: outcrop study and petroleum indication. Proc. 35th Ann. Conv. Indon Geol. Assoc. (IAGI), Pekanbaru, p. (Poster abstract) Suparka, M.E. (1988)- Studi petrologi dan geokimia kompleks ofiolit Karangsambung utara Luh Ulo, Jawa Tengah, Evolusi geologi Jawa Tengah. Doct. Thesis, Inst. Teknologi Bandung (ITB), p. 1-181. (Unpublished) (‘Study on petrology and geochemistry of North Karangsambung ophiolite, Luh Ulo, geological evolution of Central Java’. Karangsambung area (C Java) ophiolite consists of harzburgite, serpentinite, lherzolite, gabbro, diabase and pillow basalt. Originated from tholeiite magma from N-type mid oceanic ridge basalt. Radiometric ages of basalt and diabase 85.0 ± 4.3 Ma and 81.3 ±4.1 Ma.Mica schist ~85 and 102 Ma. Ophiolite result of thrusting part of mid oceanic ridge from Indo-Australia oceanic plate onto Eurasian continental plate in Late Cretaceous-Paleocene) Suparka, M.E., S. Martodjojo & R. Soeria-Atmadja (1990)- Cretaceous- Early Tertiary magmatic belt in Java: and its surrounding areas. In: Pros. Persidangan Sains Bumi and Masyarakat, Univ. Kebangsaan Malaysia, Kuala Lumpur 1990, p. 81-91. Suparka, M.E. & R. Soeria-Atmadja (1991)- Major element chemistry and REE patterns of the Luk Ulo ophiolites, Central Java. Proc. Silver Jubilee Symposium on the dynamics of subduction and its products, Yogyakarta, LIPI, p. 204-218. Suparka, S., K.H. Thio, S. Hadiwisastra & S. Siregar (1979)- Suatu tinjauan mengenai batuan metamorf di daerah Cihara, Bayah, Jawa Barat. J. Riset Geologi Pertambangan (LIPI) 2, 1, p. 1-6. (online at: http://pustaka.geotek.lipi.go.id/wp-content/uploads/2016/02/Riset-Vol.2-No.1-2-2-.pdf) ('A review of the metamorphic rocks in the Cihara area, Bayah, West Java'. Actinolite chlorite schist, hornblende schist, micaschist and granodiorite gneiss N of Cihara granodiorite, W Of Pelabuhan Ratu. Interpreted as cataclastic metamorphics of E-W transcurrent fault) Supriatna, S., L. Sarmili, D. Sudana & A. Koswara (1992)- Geologic map of the Karangnunggal Quadrangle, Java, Quad. 1308-1, 1:100,000. Geol. Res. Dev. Centre (GRDC), Bandung. Supriyanto & A.M.T. Ibrahim (1993)- Model pertumbuhan sembulan karbonat akibat progradasi sesar naik di bagian Selatan cekungan Jawa Barat Utara. Proc. 22nd Ann. Conv. Indon. Assoc. Geol. (IAGI), Bandung, 2, p. 1162-1174. (Onshore NW Java Miocene Upper Cibulakan and Prigi Fm carbonates development) Suratman (1997)- Iodiom di Cekungan Jawa Timur. Proc. 26th Ann. Conv. Indon. Assoc. Geol. (IAGI), p. 140152. ('Iodine in the East Java Basin') Suratman, R.P. Koesoemadinata & E. Suparka (1994)- Stratigraphic sequence and carbonate diagenesis of the Paciran Formation, Northeast Java basin. Proc. 23rd Ann. Conv. Indon. Assoc. Geol. (IAGI), Jakarta, p. 19-32. (Pliocene Paciran Fm limestone on Tuban High unconformable on early M Miocene Tuban Fm. Two caliche horizons subdivive formation into three sequences. Discussion of diagenesis) Suratman & S. Musliki (1996)- Anggota Ngrayong sebagai endapan regresif yang berprogradasi kaerah selatan. Proc. 25h Ann. Conv. Indon. Assoc. Geol. (IAGI), Bandung, p. 262 - 274. ('The Ngrayong member as regressive deposit of a south prograding system'. NE Java Middle Miocene sands) Bibliography of Indonesia Geology, Ed. 6.0 142 www.vangorselslist.com Sept 2016 Surono (1992)- The stratigraphic relationship between the Punung and the Wonosari Formations, Central Java. Geol. Res. Dev. Centre (GRDC), Bandung, Bull. 15, p. 31-37. (M Miocene Punung and Wonosari limestones of S Mountains of C Java can not be differentiated and proposed to be united in one unit) Surono (2005)- Sedimentology of the Paleogene Nanggulan Formation, West of Yogyakarta. J. Sumber Daya Geologi 15, 1 (148), p. 75-82. (M-L Eocene Nanggulan Fm 250m outcrop section in Kunir River, Pendoweredjo Village, 21km W of Yogyakarta. Middle part delta plain environment, upper 30m shallow marine. Volcanic materials most common in Nanggulan Fm sandstones) Surono (2008)- Sedimentasi Formasi Semilir di Desa Sendang, Wuryantoro, Wonogiri, Jawa Tengah. J. Sumber Daya Geologi 18, 1, p. 29-41. (‘Semilir Fm sedimentation in Sendang village, Wonogiri, C Java’. Volcanic Semilir Fm widely exposed in S Mountains. Overlies Butak Kebo Fm and overlain by Nglanggran Fm. Composed of sandstone, lapilli tuff and pumice breccias. Calcareous clays with nannofossils of E Miocene age. Zircon fission track in pumice breccia suggest ~16-17 Ma age, end of E Miocene. Depositional environment shallowing upward) Surono (2008)- Litostratigrafi dan sedimentasi Formasi Kebo dan Formasi Butak di Pegunungan Baturagung, Jawa Tengah Bagian Selatan. J. Geologi Indonesia 3, 4, p. 183-193. (online at: www.bgl.esdm.go.id/dmdocuments/jurnal20080401.pdf) (Oligocene- E Miocene ‘Old Andesite’ volcanics outcrop E-W along N foot of Baturagung Mountains, S Central Java. Early Oligocene Nampurejo basaltic pillow lava overlain by Late Oligocene Kebo Fm sandstone, siltstone, tuff, and shale and E Miocene Butak Fm polymict breccia with sandstone, shale, siltstone. Volcanics all deposited in marine basin. Volcanism most active during upper Kebo and Butak Fms) Surono (2009)- Litostratigrafi Pegunungan Selatan bagian timur daerah istimewa Yogyakarta dan Jawa Tengah. J. Sumber Daya Geologi 19, 3, p. 209-221. (online at: http://isjd.pdii.lipi.go.id/admin/jurnal/19309209221.pdf) ('Lithostratigraphy of the eastern part of the Southern Mountains in the Yogyakarta area and East Java'. Southern Mountains of C Java intensive volcanic activity in Late Oligocene- E Miocene. Middle-Late Miocene widespread carbonate platform deposition) Surono M & R. Fakhruddin (2014)- Sedimen pasang-surut di Kali Keruh, Desa Lor Agung, Kabupaten Pekalongan. J. Geologi Sumberdaya Mineral 15, 1, p. 41-53. ('Tidal sedimentary rocks at the Keruh Creek, Lor Agung village, Pekalongan Residency'. Documentation of 194m thick measured section of Late Miocene- E Pliocene (N17-N19) age in N Central Java (Halang Fm equivalent?). With tidal flat sedimentary structures (but apparently also rich in planktonic foraminifera, suggesting open marine setting?; HvG)) Surono, U. Hartono & S. Permanadewi (2006)- Posisi stratigrafi dan petrogenesis intrusi Pendul, Perbukitan Jiwo, Bayat, Kabupaten Klaten, Jawa Tengah. J. Sumber Daya Geologi 16, 5 (155), p. 302-311. (‘Stratigraphic position and petrogenesis of the Pendul Intrusion, Jiwo Hills, Bayat, C Java’. Intrusive microgabbro into Gamping-Wungkal Fm with Late Eocene calcareous nannofossils. K-Ar analyses of diabase and diorite of Pendul Intrusion of Bayat/ Jiwo Hills suggests two intrusive ages, M Eocene- E Oligocene (39.830.0 Ma) and M Miocene (17.2- 13.9 Ma). Nearby Tegalrejo Basalt 24.3 ± 0.7 Ma) Surono & A. Permana (2009)- Lithostratigraphic and sedimentological significance of deepening marine sediments of the Sambipitu Formation, Gunung Kidul residence, Yogyakarta. Proc. 38th Ann. Conv. Indon. Assoc. Geol. ( IAGI), Semarang, 16p. (On latest E Miocene (N8) Sambipitu Fm at Ngalang River section, S Mountains SE of Yogya. Thickness 223m, overlies E Miocene Nglanggran Fm volcanic breccias and grades upward into marl-dominated M Miocene Oyo Fm. Lower Member dominated by sandstone and siltstone, alternating with breccias; Upper Member siltstonemudstone intercalated with sandstone, marl and conglomerate. Lower Member deposited on tidal flat, affected Bibliography of Indonesia Geology, Ed. 6.0 143 www.vangorselslist.com Sept 2016 by sedimentation of volcanic material, deepening to inner shelf in Upper Member (NB: generally viewed as deeper water turbiditic series?; HvG)) Surono & A. Permana (2011)- Lithostratigraphic and sedimentological significance of deepening marine sediments of the Sambipitu Formation, Gunung Kidul Residence, Yogyakarta. Bull. Marine Geol. 26, 1, p. 1530. (online at: http://ejournal.mgi.esdm.go.id/index.php/bomg/article/view/31/31) (Same paper as above) Surono M., H. Samodra & Sidarto (2013)- Hubungan lembah Sadeng, cekungan Baturetno dan teras Bengawan Solo, Jawa bagian Tengah. J. Sumber Daya Geologi 23, 3, p. 153-161. ('Relations between the Sadeng valley, Baturetno basin and Solo River terraces, Solo, Central Java'. When Old Lawu erupted blocked Solo River and flooding of Baturetno basin S of Wonogiri in S Mountains) Surono, B. Toha & I. Sudarno & S. Wiryosujono (1992)- Geological Map of the Surakarta- Giritontro Quadrangles, Jawa. 1: 100,000. Geol. Res. Dev. Centre (GRDC), Bandung, 2 sheets. Suryantini & S. Ehara (2005)- Geothermal gradient study of onshore North West Java basin from petroleum wells. Proc. 3rd Int. Workshop Earth Science and Technology, Kyushu University, Fukuoka, p. 29-40. Suryantini, S. Ehara & J. Nishijima (2006)- Preliminary geothermal gradient and heat flow compilation from Western Java, Indonesia. In: Ann. Mtg. Geothermal Resources Council, San Diego, Geothermal Resources Council Trans. 30, p. 699-704. (Geothermal gradients and heat flow data calculated from 67 oil-gas and 3 geothermal wells. Heat flow in NW Java basin slightly higher than normal, from 60.8- 135.2 mW m-2. Temperature gradients 3.7- 6.6° C/100m. Very high heat flows in S part of basin. In volcanic area heat flow ~186.5 mW m-2. High heat flow outside volcanic area at border between gravity highs and lows, interpreted as faults) Susanto E.E., K. Mano, Sudijono, T. Sihombing & F. Aziz (1995)- Geology of the middle course of the Solo River between Sambungmacan and Ngawi. In: Sudijono et al. (eds.) Geology of Quaternary environment of the Solo-Madiun area, Central-East Jawa, Geol. Res. Dev. Centre, Spec. Publ. 17, p. 39-44. Susilohadi (2008)- Atlas seismik refleksi Selat Sunda. Marine Geol. Inst., Bandung, 14p. ('Atlas of seismic reflection in Sunda Straits') Susilohadi (1995)- Late Tertiary and Quaternary geology of the East Java Basin, Indonesia. Ph.D. Thesis, University of Wollongong. Australia, p. 1-169. (online at: http://ro.uow.edu.au/theses/1973/) (Study of M Miocene- Quaternary geology, stratigraphy and paleogeography of NE Java-Madura area. During M Miocene and before, the NE part of E Java Basin controlled by NE trending halg-grabens along sutures between Late Cretaceous- E Tertiary subduction systems. Little is known about basin configuration in S part of basin before M Miocene. Since Late Miocene E trending anticlinal zones developed, with Rembabg anticlinal zone between Blora and Madura as dominant structure) Susilohadi, S., C. Gaedicke & Y. Djajadihardja (2009)- Structures and sedimentary deposition in the Sunda Strait, Indonesia. Tectonophysics 467, p. 55-71. (Sunda Strait opening initiated in early Late Miocene following M Miocene onset of Sumatra fault system. Three major graben systems/ pull-apart basins: W and E Semangko and Krakatau. Prior to Late Miocene most of Sunda Strait and surroundings probably developed in non-marine environment.) Susilohadi, S., C. Gaedicke & A. Ehrhardt (2005)- Neogene structures and sedimentation history along the Sunda forearc basins off southwest Sumatra and southwest Java. Marine Geology 219, 2-3, p. 133-154. (20 seismic lines in SW Sunda arc margin between Manna and W Java show fore-arc basin structures and stratigraphy since Late Paleogene. Paleomorphology of Cretaceous continental margin persisted until Bibliography of Indonesia Geology, Ed. 6.0 144 www.vangorselslist.com Sept 2016 Oligocene and paleoshelf margin extended NW off Sumatra. Two structural events between Late OligocenePliocene. Back thrust-faulting along S border of fore-arc basin and initiation of Cimandiri FZ in Late Oligocene; Sumatra and Mentawai FZ initiated in Pliocene. Four Neogene sedimentary cycles. Volcanic activity abundant since late M Miocene. Turbidite deposition common along and seaward of basin slope during sea level lows in late M Miocene and L Miocene) Sutan Assin, N.A.D. & A.N.S. Tarunadjaja (1972)- ‘Djatibarang’, the discovery and development of a new oilfield. Proc. First Ann. Conv. Indon. Petroleum Assoc. (IPA), Jakarta, p. 125- 137. (1969 onshore waxy oil discovery 170km E of Jakarta. Reservoir Eocene- Oligocene Jatibarang Volcanics Fm, composed of >400m of sandy lithic tuffs with intercalations of andesites, red clay and basaltic intrusives) Sutanto (1993)- Evolutions geochimiques et geochronologiques du magmatisme Tertiaire de Java (Indonesie). Memoire de DEA, Universite de Bretagne Occidentale, Brest, p. 1-89. ('Geochemical and geochronological evolution of the Tertiary magmatism of Java') Sutanto (2000)- Batuan vulkanik daerah Kulon Progo, geokronologi dan geokimia. Bul. Tekmira 14, p. ('Volcanic rocks of the Kulon Progo area, geochronology and geochemistry') Sutanto (2003)- Batuan volkanik Tersier di daerah Pacitan dan sekitarnya. Majalah Geol. Indonesia 18, 2, p. 159-167. ('Volcanic rocks of the Pacitan area and surroundings'. Eocene- U Miocene volcanic edifices around Pacitan, S coast of C Java, Common island arc andesites. K/Ar ages 42-9 Ma. M-U Miocene volcanics from adakitic magma, from melting of young and hot lithospheric plate) Sutanto (2004)- Distribusi spasial dan temporal batuan gunung api Tersier di Jawa Tengah dan Jawa Timur. Jurnal Teknologi Mineral (ITB) 17, 2, p. 65-71. ('Spatial and temporal distribution of Tertiary volcanic rocks in Central and East Java') Sutanto (2008)- Geologi dan prospek geowisata Perbukitan Jiwo, Bayat, Jawa Tengah. J. Teknologi Technoscientia 1, 1, p. 111-121. (online at: http://technoscientia.akprind.ac.id/wp-content/uploads/2009/11/Sutanto_111_121-okbgt.pdf) (C Java Jiwo Hills near Bayat one of three places on Java with exposures of Pre-Tertiary and Paleogene rocks. Oldest rocks pre-Tertiary metamorphics, unconformably covered by Eocene Gamping-Wungkal Fm with Nummulites limestones. Cut by Late Eocene- E Oligocene (39.8, 33.2, 31.3 Ma) basaltic dykes. Unconformably covered by Oyo Fm calcarenite and marls. Proposal to preserve Jiwo Hills geotourism sites) Sutanto, R. Soeria Atmadja, R.C. Maury & H. Bellon (1994)- Geochronology of Tertiary volcanism in Java. Proc. Seminar Geologi dan Geotektonik Pulau Jawa, sejak Mesozoic hingga Kuarter, Jurusan Teknik Geologi, Universitas Gadjah Mada, Yogyakarta, p. 53-56. Sutarso, B. & P. Suyitno (1976)- The diapiric structures and relation to the occurrence of hydrocarbons in Northeast Java Basin. Proc. 5th Ann. Mtg. Indon. Assoc. Geol. (IAGI), Yogyakarta, 20p. Sutarso, B. & Suyitno Padmosukismo (1978)- The diapiric structures and their relation to the occurrence of hydrocarbon in North-East Java Basin. Geologi Indonesia (IAGI) 5, 1, p. 27-43. Sutomo, H. (1983)- Pengaruh tektonik pada batuan metasedimen di Sungai Lukulo sebelah timur Gunung Sipako. Proc. 12th Ann. Conv. Indon. Assoc. Geol. (IAGI), p. 255-262. Sutomo, H. (1984)- Penentuan asal-usul kuarsa pada konglomerat kuarsa di Gunung Cakaran, Bayat, Jawa Tengah. Proc. 13th Ann. Conv. Indon. Assoc. Geol. (IAGI), p. 455-461. Sutoyo (1994)- Sikuen stratigrafi karbonat Gunung Sewu. Proc. 23rd. Ann. Conv. Indon. Geol. Assoc. (IAGI), Jakarta, p. 67-76. Bibliography of Indonesia Geology, Ed. 6.0 145 www.vangorselslist.com Sept 2016 10 p. Petroleum Assoc. Geol.Klasifikasi stratigrafi Pegunungan Selatan.X. Conv.Carbonate reservoirs in North West Java onshore area.Sedimentological study of Gembong subdelta of Citarum delta complex.Middle Miocene carbonate sequence stratigraphy. Wonosari. (IAGI). Jakarta. Dev. (1991). Petroleum Assoc.000. p. Geol. (IAGI). Geol. Quad. dearah istimewa Yogyakarta dan Jawa Tengah. Jakarta. Jampang Tengah and Jampang Kulon. Yogyakarta. Chaniago & R. Late Miocene Parigi Fm) Suyanto. p. Proc. Proc. NW coast of Java. On Miocene carbonates of Southern Mountains SE of Yogyakarta. 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R.0 146 www. Jakarta 1982. & Y. Suyanto. F. Yogyakarta. Quad. Indon. K. Wonosari. (Unpublished) Suwardy. Thesis University of Wollongong.X. Dev. 61-71. Baharuddin (1992). Bandung. 15th Ann. Conv. Indon. Indon. Geol. p.The basement configuration of the Northwest Java area. Sahudi & I. Conv. Proc. T. Jawa. Suyitno.Geology of the Lumajang Quadrangle. Sumantri (1977). onshore northwest Jawa Basin. Assoc. Not much technical info) Suyoto (1992). Radiometric dates of youngest igneous rocks ~58. Res. Conv. Centre (GRDC). 507-532. Petroleum Assoc.Geology of the Turen Quadrangle. F. 11th Ann. 8 p. & R.65 Ma (Paleocene). Suyanto. Proc. T.vangorselslist. Indon.The geology and hydrocarbon aspects of southern Central Java. Kusnama. 1:100. F. shows different delta types at each of four tributaries). Assoc. 237-252. Jawa (Quad.Note on the carbonate outcrops in Krawang Selatan. (NW Java basement: igneous rocks intruding into older metamorphic rocks. A. (IPA). 13 p. Not much detail) Sutoyo & K. Centre (GRDC). Master Thesis Inst. 1607-4). p. 4th Ann. oldest metamorphic argillite dated as 213 Ma (Triassic)) Suyono. Indon. Jampang Tengah dan Jampang Kulon.Source rock distribution and evaluation in the Talang Akar formation. Jakarta. Suyanto. Hadisantono. Teknologi Bandung. Proc. 129-152.com Sept 2016 . M. Res. Assoc. Situmorang. Indonesia. Indon. present and future. Proc. Joint ASCOPE/ CCOP Workshop on hydrocarbon occurrence in carbonate formations.000. p. Ed. p. Bandung. 1. Conv. Assoc. Centre (GRDC). Sambipitu Fm spans zones N7-N9) Sutrisman.X (1983). 183-213. Conv. (1982). (IPA). Yogyakarta'.Exploration in West Java: play concepts in the past. p. C Java) Bibliography of Indonesia Geology. & Roskamil (1975). Suwarti. F. 35 p. 1607-5. Petroleum Assoc. Yogyakarta special region and Central Java'. Dev. p. p. Yahya (1974). Proc. (1982). 3.Klasifikasi stratigrafi Pegunungan Selatan daerah istimewa Yogyakarta dan Jawa Tengah.com Sept 2016 . 8p.id/publication/index. S5= N 13 S6= N14-N15.The evolution of Gajahmungkur paleovolcano. S4 = N11/N12. Proc. Wonogiri.Characteristics of gold mineralization at the Ciurug vein. ('Tertiary pollen zonation of Java') Syafri. West Java. 1. S2 = N8. and S9 = N20-Recent. (IAGI). A. SE of Yogyakarta.vangorselslist. as the reference to the revized terminology of "Old Andesite Formation". (also in J. I. Extensive karst topography indicates study area has been tropical since early U Miocene) Suyoto. I. Proc. Y. Indon. Lombok 2010. Conv. Sudradjat (2013). Mountain building of Kulon Progo not solely dominated by vertical undation force. A. Early M Miocene onset of first regression with deposition of S3 and widespread caliche in Gunungsewu area.. Motomura & K. S8 = N18-N19. (4) declining activity. Watanabe (2005). Budiadi & A. Indon. (Carbonate sequence stratigraphy of the Southern Mountains'. Polhaupessy. A. highest in latest mineralization stage in sulfide band in vein quartz) Bibliography of Indonesia Geology. 39th Ann. p.php/dir/article_detail/282) (Same paper as above) Syafrizal.T. E.B. Lelono (1994). W Java. (IAGI). second with S6 (Late M Miocene). but related to three regional tectonic stages: Meratus.esdm. Bornite only in S part of Ciurug vein at 515 m. (online at: http://ijog. p. Correlation with global sealevel changes prove no age similarities. p. 4. C. p. Indon. Assoc. W of Bogor. Geologi Indonesia 8. Central Java. (3) self-destruction by formation of caldera. I. (online at: www. Identified volcanic facies and location of paleovolcano vent. 6. Geol. Gold grades in Ciurug vein vary from 1. Resource Geology 55.Geotectonic configuration of Kulon Progo Area.87. 23rd Ann.2 to 100's of ppm. In Pacitan area angular unconformity between Oligocene volcanics and overlying quartz sandstones. Nugrahaningsih & E. still occurring today. S Mountains. Geol. Ed. A. Wiyono.Zonasi polen Tersier Pulau Jawa. S1= N7. 4. Proc. with SW-NE. Yogyakarta Special Region and Central Java') Suyoto (1994). Teknologi Bandung (ITB). p. N. Doct. p. with more basaltic rocks) Syafri. Central Java.The evolution of Gajahmungkur paleovolcano. Assoc. Indonesia.Suyoto (1992).esdm. Java) Suyoto (2005). (IAGI). Imai. Ciurug vein four main mineralization stages. 225-238. Geologi Indonesia 5. 67-76. Two major transgressions and regressions: first transgression with S1 (late E Miocene). Assoc. Assoc.Stratigrafi sekuen cekungan depan busur Neogen Jawa Selatan berdasarkan data di daerah pegunungan Selatan Yogyakarta. Geol. S. Conv. Conv.bgl. N.Sekuan stratigrafi karbonat Gunungsewu.0 147 www. Thesis Inst. Four stages: (1) submarine volcano with pillow lavas. Conv. sphalerite. (2) emergence above sea level forming volcano island. Pongkor gold-silver deposit.bgl. 4. Sunda and Java trends. Hartono (2010). 23rd Ann. Sulaksana & G. (IAGI). S7 = N 16/N 17. Sudrajat.go. Main metallic minerals pyrite. 185-190. 472-485. Second regression in early Lt Miocene with deposition of S7 and diagenesis resulting in karst topography. p. (S Mountains S of Yogyakarta nine Neogene sequence boundaries. NNW-SSE and E-W directions respectively) Syafri. 263-268. 23rd Ann. ('Stratigraphic classification of the Southern Mountains. J. with alternating lavas-pyroclastics.. Rahardjo. Geol. S3 = N9-N10. J. as a reference to revize the terminology of “Old Andesite Formation”. L.php/IJOG/article/view/168/168) (Kulon Progo Mountain elongated dome W of Yogyakarta. Proc. Geologi Indonesia 5.A. Structural elements mainly radial pattern. Sulaksana & G. dominated by pumice. Wonogiri Regency.id/index. chalcopyrite and galena. A.. PIT-IAGI-2010-231. in paprallel N-S trending epithermal veins in basaltic-andesitic breccia and lapilli tuff with andesite lava. 77. 263-268) (Evolution of Gajahmungkur E Miocene 'Old Andesite' paleovolcano in Wonogiri area. (Pongkor gold-silver mine. Hartono (2010). Yogyakarta.go. Sudrajat. p. Indon. ignimbrite breccias. indicating Early M Miocene arid climate. may have caused mud eruption) Tan Sin Hok (1934).com Sept 2016 . Wide range of zircon ages. Lagona & Nadila Novandaru (2014). p.D. W Kendeng Thrust Zone M Oligocene sandstones are volcanic arc-derived lithic arkoses. A.Miospores from the Eocene Nanggulan Formation in the Yogyakarta region. (On Pongkor young (~2Ma) epithermal gold. Shimamoto & O. p. 6. Masters Thesis. fluid inclusion microthermometry and stable isotope study of the Ciurug-Cikoret veins. Indonesia: evidence from mineralogic. East Java. Central Java.Fluid transport properties and estimation of overpressure at the Lusi mud volcano.S. p. Engineering Geol. Geol. R. K. P. High overpressure below mudstone almost lithostatic levels. Minimum depth of vein formation below the paleo-water table is ~90-130 m) Takahashi. Phoumephone. (1982). Watanabe (2007). Indon. Assoc. Y. M Miocene quartz arenites from Rembang Uplift Zone most mature sands in basin and derived from craton. hosted by M Miocene volcaniclastics. p. Harijoko. Late Cretaceous (60-92 Ma). S Mountains M Eocene-E Oligocene lithic subarkoses and lithic arkoses with detrital zircons from Eocene (37-46 Ma). 73-85. also Triassic (204-252 Ma) and Proterozoic (1754-2385 Ma). in andestic and dacitic host rocks. T. 303-326. Imai & K. (Unpublished) (E Java Basin sandstones volcaniclastic to lithic subarkose to quartzose. like Yogyakarta earthquake. Resource Geology 57. Trans. 2. 1.Provenance of quartz-rich sandstones deposited adjacent to the Tertiary Java Arc. 100km E of Pacitan. p. Small stress fluctuations. Japan. (2006). I Wayan Warmada. Late Miocene Upper Halang Fm facies associations of deep-sea fan. Palaeont.T. East Java Basin. Kumbang breccia above Halang Fm massive and disorganized fragments derived from volcano.Evolusi stratigrafi. 17 of which are new) Takahashi.jp/dspace/bitstream/10069/16852/1/tpps126_303. Schersten & L.Epithermal gold mineralization in the Trenggalek District. M Triassic (224-240 Ma) and Proterozoic (1084-1998 Ma). ('On microspheric Lepidocyclinas from Ngampel (Rembang. with immature sands. Page (2014). Soc. and with low salinity. University of Wisconsin.0 148 www. Conv. Jakarta.S.E Pleistocene U Kalibeng Fm source of mud at Lusi mud eruption. Plugs are subalkaline tholeiitic basaltic-andesite to calc-alkaline andesite in composition. Gold mineralization in N prospects took place in shallow marine to subaerial transitional environment (130-165 m below paleo-water table at Sentul prospect)) Tampubolon. A.volcanics. A.S. Permeability of U Kujung Fm limestone two orders of magnitude larger than Lower Kujung Fm limestone. Indonesia..lb. 126. (online at: http://naosite.silver deposits at NE flank of Bayah dome. A. R. Mitteljava). Tampubolon. (Mudstone of Late Pliocene.. Tadai (2010). (Gold-mineralized quartz veins at Trenggalek district of S Mountains Range in E Java. C Java)'. J.Syafrizal. p.W.E Miocene sandstones volcaniclastic litharenites with zircon ages mainly Late Cretaceous (70-85 Ma). Overlain by Pliocene Tapak Fm with limestones and siliciclastics of shelf and tidal flat facies) Tang. facies analysis and geochemistry of Mio-Pliocene sediments in the Banyumas basin'. Shingo. Early Mesozoic. H. (Stratigraphic evolution.pdf) (Palynology study of 48 palynomorph types in M Eocene lignite at Nanggulan.Origin of ore-forming fluids responsible for gold mineralization of the Pongkor Au-Ag deposit. Overpressure mainly caused by thick low-permeability sediments Upper Kalibeng Fm and high sedimentation rate. with some Tertiary.E. E Miocene sandstones are lithic subarkoses with recycled orogenic signature from uplift of local basement and older sandstone. K.O. 149-166. 43rd Ann. West Java.3 Ma. 1-299. De Ingenieur in Nederlandsch-Indie (IV). 136-148. A. analisis fasies dan geokimia dari sedimen Mio-Pliosen di cekungan Banyumas. and Proterozoic ages) Tanikawa. 2-3-211. suggesting input from volcanic arc and distal cratonic source.nagasaki-u. Indonesia. with zircons mainly Cretaceous (73-141 Ma). Mineralization of precious metal ore zone at fluid temperatures between 180-220°C. L. Ar-Ar age of vein ~16.6 Ma. A. mainly Cretaceous (64-128 Ma).vangorselslist. 12. Watanabe. located near andesitic plugs of 200-300m diameter.ac. Imai. Setijadji. Late Oligocene.A. Large microspheric Lepidocyclina from Lusi River near Ngampel. Resource Geology 64. 116. Madison. R. Proc.collected by Ter Haar. Paleozoic. 10p.Uber mikrosphare Lepidocyclinen von Ngampel (Rembang. Baskoro. N. 2. PIT IAGI 2014-245. assigned to Lepidocyclina papulifera Douville) Bibliography of Indonesia Geology. Sakaguchi. with lowest permeability of all samples. Idrus. crystal tuff in limestone-pyroclastic rock sequence ~15. (IAGI). indicating minor cratonic input to arc-dominated sediments.. Proc. A. M. Ed. Wibowo. pilow basalts).000. 136138. p. (1935). magnetite). also zircon. Miocene sandstones from Tegal. Scale 1: 100.. 9-18.E.Geologische kaart van Java. Java 1929. 6th Ann. Sumadirdja & P. Heavy minerals of Eocene quartz sst of Bayah.Note on the occurrence of Miogypsinoides Yabe and Hanzawa in Oligocene deposits. C. but those from NW and E Java mainly detritus from old rocks in N (Sundaland). Batavia.go. Imperial Academy. Petroleum Assoc.Heat flow measurements in the Tertiary basin of northwest Java. Co-ord.Zwei neue mikrosphare Lepidocyclinen von Java. M Miocene sandstone from N Bantam with zircon.vangorselslist. 11 p. C. 1:100. p. Res. Thamrin. Prayitno (1982). C.W. Richards (1975). M. & S. Fourth Pacific Science Congress. Dienst Mijnbouw Nederlandsch-Indie. Said. ('On Leidocyclina gigantea Martin from S Priangan (W Java). a stellate form from W Java) Tan Sin Hok (1943). brookite). metamorphic rocks (including glaucophane schist.com Sept 2016 .Geologic map of the Magelang and Semarang quadrangles (11-XIV-B. Bumiayu district of Tegal Residency. De Ingenieur in Nederlandsch-Indie (IV). Conv. volcanic breccia zone and Turritella Marls (mammal fauna now interpreted as E Pleistocene Satir 'island fauna'. Indon. hypersthene. which contain rhinoceros. C Java..The status of the melange complex in Ciletuh Area. 6. p. De Ingenieur in Nederlandsch-Indie (IV). gabbro. staurolite. Excursion Guide E4. Jakarta. ('Notes on the sediment petrography of Java'. 50 p. Bone beds dip 25-40° (therefore believed to be possibly of Pliocene age) and underlain by thin-bedded Late Miocene marl.Aanteekeningen over de sediment petrografie van Java. (Geologic map and description of Bumiaya area SW of Slamet volcano. H. Tokyo. age of folding in this area is therefore post ~1. 18th Sess.jstage. Cervus. This demonstrates that Miogypsinoides made its appearance in Oligocene time (Td)) Ter Haar. Joint Prospecting Mineral Resources in Asian Offshore Areas (CCOP). from N Rembang area mainly 'old rocks' provenance (zircon. 9. andalusite. Elephas. (1933). 1-8.limestone (with Lepidocyclina (Trybliolepidina). Lep. ('Two new microspheric Lepidocyclinas from Java'. p. Proc..jp/article/pjab1912/19/9/19_9_585/_pdf) (During exploration in 1942 of Cimandiri coalfield. Comm. Proc. brookite and rare augite (mix of 'old rocks and volcanic source). Indonesia.Uber Lepidocyclina gigantea Martin von Sud-Priangan (West-Java). 1-15. anatase. (B) omphalus. De Mijningenieur 14. (1929). a sample was collected N of mouth of Tjibeuleungbeung that contains both Camerina fichteli. and a Miogypsinoides sp. accompanied by isolepidinenephrolepidine and eulepidine Lepidocyclines. Etc. Geol. Two M-L Miocene new species described. C Java and S Mountains. Dev. collected by Bothe and Lep. C. Prijomarsono (1977). Centre (GRDC). p. + map. 241-253. Java. HvG)) Ter Haar. 1996?) Thaden. 585-586. phyllite) and sheared sediments (probably Upper Cretaceous Bibliography of Indonesia Geology. SW Java rich in tourmaline.. E. 11-XIII-E). Siswoyo & S.jst. anatase. (online at: www. Bandung. 2. hippopotamus. R.) Ter Haar. E. (IPA). partly remapped as Majenang Quadrangle by Kastowo & Suwarna. tourmaline. showing complexly folded NE-directed thrusts involving Miocene rocks.. 2.000. p. (Fieldtrip guide to locality of Pleistocene fossil vertebrates in Kali Glagah. Tegal (C Java) and Bengkulu (S Sumatra)'. 19. Ed. hornblende. suggesting erosion of 'old' acid plutonic rocks. Toelichting bij blad 58 (Boemiajoe). etc. etc. W Java. rutile. 2. Proc. (B) stratifera from Pasean village. (Structurally complex mixture of ultrabasic rocks (partly serpentinized peridotite. New work confirms view of Rutten (1925) that Neogene sediments of S Java are composed of detritus from volcanic arc of S Java. staurolite. of andesitic origin (augite. South-West Java. 8.5 Ma. p. Large microspheric Lepidocyclinids) Tan Sin Hok (1935).Tan Sin Hok (1935). Thayyib S.Boemi-Ajoe District. 224-235.L. 1. Tegal (Mittel-Java) und Benkoelen (Sud-Sumatra).0 149 www. Seoul 1981. 1. Bandung. displaced 40000 people and caused >US$2. and interpreted as Holocene sea level highstand episode) Thompson..P. 51-56. p. Davies & R. E Java’.X. Possible continuation of Luk Ulo melange.. p. 385-405. Geochem. M. 24p. (Terrace of presumed beach deposits with marine fossils 1. Jaarboek Mijnwezen Nederlandsch Oost-Indie 58 (1929). Search and Discovery Art. Indon. Exhib. D. 1-13. (1930).W. Thommeret (1978). 41791. (3-D model of anomalous density for Merapi and Merbabu by inversion of gravity field) Tingay. 6. Evaluation of 5-6 thin (<1m) coal horizons in what is now known as M Miocene Ngrayong quartz sandstone Formation.. (Liptinitic kerogen yield oil at earlier level of maturity than sapropelic kerogen. (Abstract + Presentation) (Lusi mudflow S of Surabaya. (‘Report on geological investigations in Rembang Residency.5.Anatomy of the ‘Lusi’ mud eruption. Detailed descriptions of Miocene stratigraphy of area around Ngandang-Lodan anticline.Thermal maturity and oil generation with reference to the CMS-1 (Java) and Susu Selatan-1 (Sumatra) wells.searchanddiscovery. Major oil generation at vitrinite reflectance 0.4 m above present sea level along N coast of Java at Jepara. 6p.. Yangon 2015. Blowout in Banjar Panji-1 hydrocarbon exploration well was most likely mechanism for triggering Lusi mudflow) Tingay.Early Oligocene Ciletuh Fm quartz sandstones) ‘T Hoen. Optimum oil generation at vitrinite reflectance ~0. Verhandelingen.Suyanto (1979).14C datings of some Holocene sea levels on the north coast of the island of Java. Arpandi & F. In Susu Selatan-1 well (N Sumatra). C. Toelichting bij Blad XVI (Midden Java). has been erupting continuously for 9 years. Heidbach. 150m away). Tingay. Indonesia. Modern Quaternary Research in Southeast Asia 4. & Y.G. ASEG Conf.8%/ spore colour index 7.P. p.pdf) Bibliography of Indonesia Geology.) Thommeret.CMS-1 well (onshore NW Java) heavy waxy oils generated from liptinitic kerogen. Similar coal-bearing series in Panowan-Kadjar anticline WSW of Lodan) ‘T Hoen. light oils generated from sapropelic kerogen. O. Ed.35% and spore colour index 3-3. p. O.Triggering of the Lusi mud eruption: earthquake versus drilling initiation. This study suggests drilling kick. R.shales) probably melange complex. M. No heavy oil accumulations in this area) Tiede.55%/ spore colour index 5. R.W. Jaarboek Mijnwezen Nederlandsch Oost-Indie 45 (1916). Geoph..vangorselslist. 6.P. Swarbrick (2008).5. or natural event induced by 2006 Mw6.The Lusi mud eruption of East Java. Davies & R. Gerstenecker & J. 250km away). E Java.0 150 www. (2016). C. Indonesia. Rel. A. Geosys. 639-642. with detailed crosssections across Ng-Lodan anticline. 9. East Java. (G3). C. Fernandez (2005). Dated as 5000. Jakarta.3650 years B. M.A. Heidbach.000. Ongoing debate whether the disaster was triggered by drilling kick in Banjar Panji-1 well (1 day earlier.Geologische overzichtskaart van den Nederlandsch-Indischen Archipel 1:1. not earthquake.A.. Onset of oil generation at vitrinite reflectance 0. (IPA). 370 km to E. Proc. M. (Lusi mud volcano in E Java unlikely to be triggered by Yogyakarta earthquake. Petroleum Assoc. J. Proc. AAPG Int. 8. caused catastrophic shear failure of borehole wall and subsequent reactivation of Watukosek fault) Tingay.7 billion in damage. (2010). 33p. p.net/documents/2009/50187tingay/ndx_tingay. (1918).000. via the inverse gravimetric problem.3-2.com Sept 2016 . (Extended abstract and presentation) (Online at: www.3 Yogyakarta earthquake (2 days earlier.What caused the Lusi Mudflow disaster in Indonesia? In: 2nd AAPG/EAGE/MGS Conf.Modelling the density at Merapi volcano area. Verhandelingen 2.. Camacho. S.. Sydney 2010. Geology 36. C. 1-72.Verslag over de uitkomsten van een geologisch-mijnbouwkundig onderzoek in een gedeelte der Residentie Rembang. NW Rembang zone. 8th Ann. (Explanatory notes for 1929 1: 1 million scale geologic overview map of Central Java. 202-254. p. Swarbrick (2009). Conf. Cape Town 2009. Overlain by M Eocene. Innovation in geoscience: unlocking the complex geology of Myanmar. Conv. Trybliolepidina. 2. Wang (2015). Bull.Paleo-current and initial slope indicators in the Subang area. H. p. West Java. Dept. p. p. H.D. p. To N uppermost limestone beds overlain by and interfingering with beds of Marl-tuff Mb of Tertiary f3. Mining Institute of Japan 58. K.php?li=article_detail&id=847) ('Notes on the stratigraphy of the Karangbolong Mountains. Dept. Oldest rocks 'Old Andesite Fm' composed of Oligocene.Aquitanian andesitic eruptive and intrusive rocks. Km-long linear ridge are relics of paleo-breaker zones.D.Origin of Tjongkang Hill near Tomo. Bibliography of Indonesia Geology. Contrib. with horizontal displacement of ~140 m. H. H. West Java. C Java'. M. Teknologi Bandung (ITB) 1. Technology Bandung (ITB).450m) Tjia. 63-74. 7. H. p. 75-88. M. 75.). (1962). engulfing 8 villages) Tingay.(‘Lumpur Sidoarjo’ mud eruption probably triggered by drilling of Banjar Panji 1 well in May 2006.jp/article/shigentosozai1885/58/685/58_685_309/_pdf) (Brief review of NE Java basin stratigraphy and oil fields)) Tjia. Geologi Indonesia 8.id/index. Geol.Structural analysis of the Pre-Tertiary of the Luk-Ulo area.Initiation of the Lusi mudflow disaster. C Java) Tjia. (online at: http://idci.go.D. 6. Pleistocene S-ward tilting of island (<4°).php/IJOG/article/view/157/157) (Review of landforms in karst hills in Miocene limestone of Southern Mountains SE of Yogyakarta. (online at: http://journal. H. Djawa Tengah.J. (1961).jstage. (2013). (1968). 309-316. W. probably of Late Miocene age.Tjatatan mengenai stratigraphy Pegunungan Karangbolong. W of Tjikapundung valley. Survey Indonesia 1. 60p. 683-686.go. in accordance with paleomagnetic data) Tjia. etc.itb.Oil-fields in Java.Morphostructural development of Gunungsewu karst. East Java. After this time marine sedimentation in this area came to halt) Tjia. Cycloclypeus spp. J. M. America (GSA) Bull.vangorselslist. Geology 63.Y. 89-98. 126-130. Jawa Island. 57. H. (1964). Proc.Topographic lineaments in Nusa Barung. (In Japanese) (online at: www. 10 km N of Bandung.D. R. N-ward facing scarp exposed over 22 km. Geology Inst. 3.id/index. J.jst.bgl. 685. Mud flow now covers >700 ha of land to depths of up to 17 m. (Lembang fault. 2.D. (On slickensides in Lokulo area. Davies & C. (1964). unconformably overlain by Karangbolong Lst (Tf1-3. Java. Also circular and spiral landforms. & V. (online at: http://ijog. Tjia. cone-and sinoid-shaped.esdm.com Sept 2016 . Geol. parallel to Java's longitudinal axis.Slickensides and fault movements. Ed. E part of fault between Maribaja and Mount Pulusari is dip slip fault with exposed throws of 130. Karangbolong Mts part of Java S Mountains. (Repeat earlier conclusions that 'Lusi' mudflow eruption S of Surabaya was not triggered naturally but was consequence of Lapindo drilling operations) Titani.000 m3/ day. Expelling mud up to 170. (1966). Geologie en Mijnbouw 47. Former investigators attributed mainly dip slip displacements to this fault.id/pdf/JURNAL/ITB%20Journal%20of%20Science/ ) (Nusa Barung island off Puger at S coast of E Java mainly N-S trending karsted limestone ridges. Inst.The Lembang Fault.D.ac. Tjioe (1964). 110p. Proc. H.. Teknologi Bandung (ITB) 2. 18-22. Inst. Technology Bandung (ITB).dikti. similar to most of S Mountains) Tjia.go.D. Some arenites of Lower Pliocene unit deposited by turbidity currents) Tjia. (Pliocene deposits of Subang area with sedimentary structures indicating currents mostly longitudinal. Changes in orientation of inland and coastal ridges interpreted to reflect progressive CCW rotation of Gunungsewu microplate. Contrib.D. 493-494. but W part of fault.0 151 www. Central Java. (1942). Rudolph.L. latest development sinistral strike slip in nature. p. Nature Geoscience 8. Soc. Inst. p. 2. Manga. p. with Nephrolepidina. suatu kontribusi. Tuban. Twnenty-one coral species. 19-36. Agustiyanyo & M.1. 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Purbo Hadiwdjojo (1992).5km NE of Slahoeng. 26.nl/DL/publications/PU00017948.Het ontstaan van het Dieng Plateau. 3. (IAGI). Kabupaten Kebumen. Stratigraphy in area Late Oligocene.iatmi.id/uploads/IATMI_2007-TS-03_Bambang_Triwibowo. 1210-1. Toha. Soetoto. UPN. 131-149.Potensi dan kualitas batuan Formasi Kujung sebagai batuan induk. 1:100. Kolokium Hasil Kegiatan Inventarisasi Sumber Daya Mineral. Jawa Timur. The elevated Dieng Plateau of C Java is not caldera formation or crater bottom. 14p. Indon. Associated with Aceratherium boschi rhinoceros tooth (oldest land mammal fossil known from Java). (online at: www. Res. Proc. 1209-4. Ayah area. 47% still living.26. (online at: http://elib. Sidarto.90m thick. B.pdf) (Reefal limestone lenses in U Halang Beds along Cisande River. Y. ('An occurrence of zinc-ore in South Madiun'. Subagyo (1994). McCaffery. (online at: www. Geol. 44-51. Ed. W Java. but floor of an old mountain lake. 2135-2138. Oil content 7.Geology of the Jakarta and the Thousand Islands Quadrangle. M. maybe around Mio-Pliocene boundary) Bibliography of Indonesia Geology. p. Proc.Geologi daerah Pegununungan Selatan. J.repository. De Mijningenieur 2. p.E Pliocene Halang Fm turbidites and Late E Miocene. & C. In: Proc.F. B. Kon. Brunner. R. Bitumen resources is ~ 830. (1930). suggest convergence at 67 ±7 mm/year orthogonal to trench) Triwibowo.3.M.O. 6. Java.. Nas.M Miocene andesitic intrusives Solid bitumen/oil shale deposits in Kalipucang Fm.pdf) (Investigation of solid bitumen/oil shale in M Miocene Kalipucang Fm. W. B. 13p.O. Nederl. p.go.Een zinkertsvoorkomen in Zuid-Madioen.Corals from the Upper Miocene of Tjisande. (2003).A. C. Central Java. Geol. Setiawan (2001).vangorselslist.nl/DL/publications/PU00018197. Publ. Teknik. Klaten. p. 1-11. 87-93.com Sept 2016 .E. T. 2. Geol. 1. p. J. Conv. Ann. Geol. p. W Jiwo. Unusual erosional features on limestone plateau) Umiyatun Choiria. M. Discocyclina spp. Ruswandi (1973). M. ('Structural pattern of Java and Madura as a result of preliminary interpretation of gravity data') Uruma.pdf) (35 coral species from Late Pliocene Upper Kalibeng Beds at Sonde in W part Kendeng zone. A. 1-207..Gravity survey in the Yogyakarta. Paleontology 20. collected by members of Geological Survey) Umbgrove. Proc. (1950). Java'. Untung. 6. Udjang & E.F. Survey Indonesia and Geol.The claystone age of Wungkal Formation based on calcareous nannofossils in Gunung Pendul area. Pekanbaru. Geol. Geol.. Sato (1978). Verhandelingen Kon. PIT IAGI2006-072.Foraminifera besar pada satuan batugamping Formasi Gamping. 5th Int. Untung. Nederl. IAGI) 9. Sekarbolo. 49. Proc. Ed.Pola struktur Jawa dan Madura sebagai hasil penafsiran pendahuluan data gayaberat. & Y. p.Gravity and geological studies in Java. Watanabe.preserved coral fauna of 70 species) Umbgrove. is Lower Pliocene patch reef in marly Tapak Beds. Geologi Indonesia (IAGI) 2. 2.. p. Publ.0 153 www. Yogyakarta. N. 521-542. Res. E Java..Wungkal Fm. Bayat. (Small hill of Gunung Linggapadang near Prupuk. Bibliography of Indonesia Geology.. 6. Imai. Survey Indonesia. Serie 9.Sebuah rekonstruksi paleogeographi Pulau Jawa. Indonesia. Indon. Kon. Conv. L. Geol. 15-24. E Java. 637-651. ('Larger foraminifera from limestones of the Gamping. ('Java's south coast near Tji-Laut Eureum'. Bayat. & G. K. p.H. J. p. Dev. Cosijn (1931). C Java. Prastistho.000. M.Corals from the Upper Kalibeng beds (Upper Pliocene) of Java. 30th Ann. Setijadji & A. (Forty species of corals from lower Pleistocene Pucangan beds of Kendeng zone. Reef comparable to patch reefs in Bay of Jakarta. pengaronensis. (1974). Central Java. J. M. 6.Java's zuidkust bij Tji-Laoet-Eureum. Spec.H. Y. Geol. J. with only 49% living species. Geofisika 3. (1982).Corals from a Lower Pliocene patch reef in Central Java. Untung. Well. K. Geologisch Mijnbouwkundig Genootschap (KNGMG). and Spiroclypeus vermicularis) Umiyatun Choiria. p. M. 133-134. p. Assoc. This abnormally low percentage probably due to special character of fauna which consists mainly of solitary 'deep water' corals) Umbgrove. p. Assoc.H. Proc. Indon.F. Indon. Survey Japan.000 (2 sheets). J. Bandung. Jawa Tengah. N. Bayat Klaten. Nederl.Wonosari area. Assoc. S. 15-24. Fukuoka. 377-384.Corals from the Putjangan beds (Lower Pleistocene) of Java. Workshop Earth Science and Technology. 6. Harijoko (2007). Untung.Bouguer anomaly map of Jawa and Madura. Jiwo Barat.dwc. & J. Ser. Jati Kurniawan & Surono (2006).. J. 1. (online at: www. Pellatispira orbitoidea. S. (IAGI) and 10th GEOSEA Conv. Untung. Amsterdam. & J.F. (1946). Scale 1:1. M-U Eocene (zone Ta3) larger forams from classic Jiwo Hills locality include Nummulites javanus. (1946). Centre (GRDC). Kohno. Akademie Wetenschappen.Umbgrove.H.Wungkal. Paleontology 24. R.Migration of subduction in Central Java. Itya. (IAGI). Assilina spp. Wiriosudarmo (1975).F. djokdjakartae. In: Proc. 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(On N Central Java basin (N Serayu Basin) pull-apart basin evolution and oil seeps) Usman. ('Source rock potential in the Majalengkah area and implications for hydrocarbon rock potential of the Bogor Basin'. Jakarta. 3. M.Ein Beispiel fur Sekundartektogenese auf Java. (Unpublished Report) (Explanatory notes to Geological map of Java. (1937). Toelichting bij Blad 36 (Bandoeng). Panguriseng & W. Issue (163)... with dykes. Surabaya. 55-65. 35-46.sheet 36 (Bandung)) Van Bemmelen.K. Modjo (1982).New concept of Paleogene basin evolution of northern West Java. T. p.000. S. ('The Cisubuh Formation as hydrocarbon reservoir rock in the NW Java and North Central Java basins'. R. H.J.S. 7p. Bull. T. NE of Pacitan near C-E Java border. 81-87. M. De Ingenieur in Nederlandsch-Indie (IV Mijnbouw en Geologie).0 154 www. Bronto & L. R.Potensi batuan induk di daerah Majalengka dan implikasinya tehadap keberadaan hidrokarbon di daerah cekungan Bogor. 35th Ann.000.W.Petrologi dan geokimia batuan gunung api terubah daerah Ponorogo. Prasetya (2006). pillow lavas..Formasi Cisubuh sebagai batuan reservoir hidrokarbon di cekungan Jawa Barat Utara dan Jawa Tengah Utara. Indon. T. ('Petrology and geochemistry of volcanic rocks in the Ponorogo area. Kamal & W.K. etc. 5p. 175194. (Andesites from NE of Bandung show Late Paleocene (59± 2 Ma) and Late Eocene (37± 4 Ma) ages. Van Bemmelen.. (IAGI). PITIAGI-026. Conv. Dirk. Purnomo & P. Naskawan. R. Indon. Geochemical/ biomarker study of rocks and oils from area near first oil well on Java. Conv. mainly andesitic. (1934). Yuliandri. Conv.Early Pliocene Cisubuh Fm oil bearing in wells Jatirarangon 2 and 3 and Klantung-1) Usman.. Late Oligocene Rajamandala Fm is equivalent to Pondok Makmur Fm in NW Java. possibly oldest volcanic rocks in region) Uyeda. IPA11-G-116. Proc. p. (NW Java Basin basin evolution tied to S-ward shift of position of Indian Ocean subduction system from Jurassic to present-day. (IAGI) and 30th Ann.com Sept 2016 . p. Jawa Timur.J. Indon.Usman. Conv. E. Geol.K. T. Petroleum Assoc. S. De Ingenieur in Nederlandsch-Indie (IV). large Lepidocyclina. Volcanic necks probably of Late Pliocene age. converted into fine-grained marble. The Hague.The volcano-tectonic structure of the Residency of Malang (Eastern Java) (an interpretation of the structure of the Tengger Mountains.000. (1941).Geologische kaart van Java. as known in late 1940's) Van Benthem Jutting. Four small areas with Eocene outcrops) Van Bemmelen. (1937).. (Discussion of E Java between Madura Straits and Indian Ocean and the Arjuna. 9.nl/document/149951) Bibliography of Indonesia Geology.). 6.knaw. etc.com Sept 2016 . became connected with mainland. 9-18. p.659. De Ingenieur in Nederlandsch-Indie (IV) 7. 1-116.W. 171-194. Toelichting bij Blad 73 (Semarang) en 74 (Oengaran).W. (1937). (1938).Java. 50.De Ringgit-Beser. Volcano grew above sea level. (‘Granitic intrusions in the Southern Mountains of West Java’. p. Ringgit-Beser volcanic complex originated in shallow sea at N coast of E Java during Plio-Pleistocene. (1941). een geplooide alkali-vulkaan in Oost-Java. Van Bemmelen. Zoologische Mededelingen 20. 2. p. (online at: www. C.W.W. T. p.Tengger and Lamongan volcanic complexes) Van Bemmelen. Proc. belonging to (M Miocene) Rembang layers) Van Bemmelen. (1940). Nijhoff. Toelichting bij Blad 66 (Karangkobar). Government Printing Office. 7. R.W. Semeru.Geologische kaart van Java 1:100. Kon. p. 3. Amsterdam..Bromo. 50 p. with 1-2 cm reaction rim with secondary minerals) Van Bemmelen. R. 115-135. at N foot of Ciremai volcano~ 20 km W of Cirebon. (Major review of Java geology. (1947). (1937).Non marine mollusca from fossil horizons in Java with special reference to the Trinil Fauna. 4. 1. (Kromong Mountains formed by complex of volcanic necks up to 587 m high. R.repository.A limestone block in hyperstene dacite from the Koeda-neck (Kromong Complex. (online at: www. R. Natuurkundig Tijdschrift Nederlandsch-Indie 98. Dienst Mijnbouw Nederlandsch-Indie. De Ingenieur in Nederlandsch-Indie (IV). Nederl. 8.At SE side large limestone inclusion on top of dacitic Koeda-neck. p.nl/DL/publications/PU00018362. p. 4. Volcanics of Rahtawu cauldron large inclusions of contactmetamorphic limestones with Katacycloclypeus annulatus. with original descriptions of Penyaten Fm. Probably part of 'Old Andesites' complex) Van Bemmelen.000. 6. R.dwc. Limestone with Miocene foraminifera exposed as uplifted blocks at NE and SE side of complex. 159-172. (Explanatory notes for Semarang and Unguran 1: 100. 1:100. etc. Bandung. Akademie Wetenschappen. In: The geology of Indonesia. 653-658. Two examples: quartz-dioritic intrusion in Tjilajoe River.W.W.The Muriah volcano (Central Java) and the origin of its leucite-bearing rocks. and was subjected to folding in younger Pleistocene (Beser Ridge anticline)) Van Bemmelen. R. Ed. intrusive in Miocene limestone and MioPliocene marine sediments (Kaliwangoe-series). R. Java) Van Bemmelen. R. 83-180. 37-41.vangorselslist. (1937).Igneous geology of the Karangkobar region (Central Java) and its significance for the origin of the Malayan potash provinces. p.000 Geologic map sheets.W.W. 60 km S of Bandung and Tendjolaoet Ridge granodioritic intrusion 40 km SSW of Tasikmalaya.pdf) (‘Mediterranean-type’ leucite-bearing rocks of Muriah volcano formed from limestone assimilation by ‘Pacifictype’ magmas.Van Bemmelen. near Cheribon. p. (1949).Granitische intrusies in het Zuidergebergte van West Java. Western Java).0 155 www. 545. a folded alkali-volcano in East Java’. (‘Ringgit-Beser. (C Java Ungaran region. R. De Ingenieur in Nederlandsch-Indie (IV).naturalis. Dienst Mijnbouw Nederlandsch-Indie. East Java. introduced for specimens with multilepidine embryon) Van den Hoek Ostende. I. D.Oligo-Miocene Lepidocyclinas and planktonic foraminifera from East Java and Madura. (1923). 5. p. Bringin and Gegunung oilfields. mainly subgenus Nephrolepidina. J.Cenozoic Molluscan types from Java (Indonesia) in the Martin Collection (Division of Cenozoic Mollusca). Indonesia. Geophys.B. var. Lepidocyclinas 'grade of enclosure' increases systematically from 36% to 65% up section.knaw.Variation in forearc basin development along the Sunda Arc.De stratigrafie van het Tertiair van Java.W. followed by basin and slope sediments derived from evolving magmatic arc. Burton.E.. Geochem. Forearc basins initially with submarine fan deposits. Contains 5700 type specimens of 912 species) Vanderkluysen.P.knaw. Lepidocyclina wanneri n. Proc.Smekens (2014). Akademie Wetenschappen 52.repository. (LUSI mud volcano in E Java erupting since 2006. L. Wesselingh & C. Elbert and Selenka and Bandung Geological Survey. no stratigraphic context) Van der Vlerk.Lepidocyclininae from Rembang (Java) with a description of L. 4. M. H.P.Composition and flux of explosive gas release at LUSI mud volcano (East Java.5% CO2. (online at: www. Kon. Southeast Asian Earth Science 14.com Sept 2016 . Leiden. 53-56. Nederl. Last few years of activity characterized by periodic shortlived eruptive bursts.)) Van den Abeele.dwc. Techn. Seven Lepidocyclina species. Leloux. p. J. Indonesia. wanneri n. Akademie Wetenschappen. p. Java: Lepidocyclina rutteni n. 5.vangorselslist. De Ingenieur in Nederlandsch-Indie 4.0 156 www. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederlandsch Oost-Indie 1. Martin collection at Naturalis Museum. 760-765. Mus.R.naturalis. Kon. Kon.F. from Nyalindung beds near Sukabumi) Van der Vlerk. L.pdf) (129 species of mainly deeper marine foraminifera in Pliocene marls.M.Young Tertiary smaller foraminifera from the neighbourhood of Ngimbang. S of Java. In Miocene. National Museum of Natural History.A. Viviparus. 392-399. 331-349.5% methane) Van der Sluis. Geosystems 15. 70. Nat. p. Nederl.R. p. etc. Leiden.sp. SE of Rembang. (1996). de Vletter (1942). p. (Composite section of Oligo-Miocene sediments of E Java and Madura with Lepidocyclinas and planktonic foraminifera. (1949). I. (online at: www. (Online at: www. Winkler Prins (2002). 7. A. Molluscs from same samples described by Wanner & Hahn (1935). Present forearc basin configuration initially controlled by extension and differential subsidence of basement blocks in response to Late Eocene India-Asia collision. F. Natuurhist.. 6.. p. (1924).M. Proc. 16-35. collected by Wanner. Thiara.nl/DL/publications/PU00017817. W. mainly from Java. Samples collected by Rutten in SW corner of 109-Lamongan map sheet. (Sunda Arc fore-arc areas between Sumatra and Sumba. mainly from Latest Pliocene-Pleistocene of Kendeng zone/ Trinil area. Postuma (1967). & D. sp.nl/document/45042) (Listing and re-descriptions of Tertiary mollusc type specimens in K. Ed.nl/DL/publications/PU00018695. Hartnett & J. 2932-2946. from Tji Lalang beds and Lepidocyclina/ Miogypsina/ Cycloclypeus and Rotalia beccarii atjehensis n. N and NW of Bojonegoro. & J.sp. 0. (Miocene larger forams from W. 1010-1015. Indonesia). Late Oligocene increase in convergence between SE Asia and Indian Plates associated with new pulse of subduction resulted in basement uplift and formation of regional unconformity along entire Sunda Arc. Proc. OligoMiocene boundary placed above Globigerina ciperoensis ciperoensis zone) Van der Werff. Van der Vlerk. Lymnaea. 1-130. Incl..dwc. B. 7.(Monograph of fresh water molluscs from collections of Dubois. No location map. Corbicula.M. Gases sampled 98% water vapor.F. Bull. 1. J. I. Incipient collision between Australia and W Banda Arc caused back-arc thrusting and basin inversion. Clarke. p.pdf) (Lepidocyclinids from E-M Miocene 'orbitoidal limestone (OK)' of Rembang Beds near Sumberan. Sumba and Savu forearc sectors characterized by forearc extension. Akademie Wetenschappen 45. Bibliography of Indonesia Geology. Nederl. 10.Foraminiferen uit het Tertiair van Java. some Multilepidina. De voorhistorische verhoudingen van land en zee in den Oost-Indischen Archipel. L. 5-76. Along Sumatra W coast uplift along inner side of forearc along older transcurrent faults.0 157 www. Jaarboek Mijnwezen Nederlandsch Oost-Indie 12 (1883).J. (1873). L. West Java. Bantam). De Mijningenieur 7. Ed. (1884). assistentresidentie Grobogan. Common andesitic intrusions) Van Es. (‘Additional data on the Bojongmanik coal field’.Geologische waarnemingen op Java. Wetenschappelijk Gedeelte 2. (‘Contribution to the knowledge of the stratigraphy of the Tertiary in the Banten Residency’ West Java. (1883). Initial forearc basin subsidence relates to age of subducting oceanic lithosphere.Geologische overzichtskaart van den Nederlandsch-Oost-Indischen archipel (schaal 1:1. Jaarboek Mijnwezen Nederlandsch Oost-Indie 1872. Jaarboek Mijnwezen Nederlandsch Oost-Indie 45 (1916). (‘Survey of the occurrence of natural oil near Purwodadi. (1918). Jaarboek Mijnwezen Nederlandsch Oost-Indie 44 (1915). 133-234. Coals thought to be too thin and poor quality for commercial exploitation) Van Es. ('Coal in the Semarang area') Van Dijk. 9. (‘Description of the marble in the assistant-residency of Pacitan’. p. (1918).C. Attempt to compare S Banten and S Sumatra stratigraphies (but poor age control). Verhandelingen 2. (1926). (1917).Bijdrage tot de kennis van de stratigrafie van het Tertiair in de Residentie Bantam. non-volcanic part of the Residency Surabaya'. Grobogan region'. 55-140. (Overview map and explanatory notes off southernmost Sumatra and W Java) Van Es. 2.C.J. 151-192. p.Over de geologie van het noordelijke. 150-153. (1872). P. (Early paleogeographic map of Indonesia at end Pliocene and its implications for migration of animal species) Van Es.C. L.C.000). Wetenschappelijk Gedeelte. Details on coal thickness and composition.Beschrijving van het marmer voorkomende in de assistant-residentie Patjitan.000. (1872). P.Nadere gegevens over het Bodjongmanik kolenveld.vangorselslist.J. Djiwo en Zuidergebergte. p. Verhandelingen 2. p.com Sept 2016 . P. Hill near Ngemba village in Lusi River valley near Purwodadi with steeply dipping Tertiary sediments. Bibliography of Indonesia Geology.J. I. (1920). 359-369. On 1992 GRDC map this is shown as E Miocene Campurdarat Fm in area with common andesitic intrusions) Van Dijk. en de invloed daarvan op de verspreiding der diersoorten. p. Jaarboek Mijnwezen Nederlandsch Oost-Indie 1873. ('On the geology of the northern. Investigation of suitability as building stone of ‘marble’ (crystalline limestone) at East side of Panggul Bay. Flexural loading of evolving accretionary prism and across arc strike-slip faulting may result in additional forearc subsidence. NE Java. P. p.Toelichting bij Blad XV (Lampongs. p. Verhandelingen 2.J.C. 193-215. L. p. 255-304. L. 164-174. Verhandelingen 1. including limestone breccia with salt water with oil seeps) Van Dijk.) Van Dijk. P. Jaarboek Mijnwezen Nederlandsch Oost-Indie 45 (1916).Steenkolen in het Semarangsche. 153-157. 6. Partly based on data rom 700+m deep well near Gresik) Van Es. p. 1.increase in size of accretionary prism and convergence rates resulted in folding/ uplift of distal forearc basin strata.Geologische beschrijving der residentie Djokdjakarta.Onderzoek naar het voorkomen van aardolie in de nabijheid van Poerwodadi. niet-vulkanische gedeelte van de residentie Soerabaja. Straat Soenda. Jaarboek Mijnwezen Nederlandsch Oost-Indie 1884. p. Jaarboek Mijnwezen Nederlandsch Oost-Indie 47 (1918). (‘Geological description of the Residency Jogyakarta’) Van Dijk. Jaarboek Mijnwezen Nederlandsch Oost-Indie 1. Southern Mountains of SE Java. Orbulina. 183-209. Discocyclina.Gastropoda. Bandung. p.repository. De Ingenieur in NederlandschIndie IV. Part II (Families Planaxidae-Naticidae inclusive).nl/document/549598) (First of series of paleontological papers on molluscs from Plio-Pleistocene Kendeng Beds W of Surabaya. etc. because more erosion on N flank of anticline) Van Es. 1987. Cerithiidae. Early Miocene volcanic breccias. Mededelingen 13. (1938).1925). suggesting Jiwo Anticline was already folded in Middle Miocene. 37. zinc).Oude exploratiewerken in Zuid-Madioen. and formed from bat excrement) Van Gorsel. 1-86. Mainly quartz veins with chalcopyrite in volcanics.T. (1942).naturalis. Paleoclimate signal inferred from fluctuations in cooler-climate planktonic forams used to correlate with Mediterranean Miocene-Pliocene boundary stratotype) Van Regteren Altena. Bibliography of Indonesia Geology. 2. Kadar & P. Van Gorsel.The marine Mollusca of the Kendeng beds (East Java).The marine Mollusca of the Kendeng beds. East Java. L.O. Van Gorsel. (Field guide to Trinil hominid site. 11. Java 1929. ('Old exploration works in South Madiun'.The marine Mollusca of the Kendeng Beds (East Java) Gastropoda.C. Gastropoda. dealing with gastropods belonging to families Planaxidae. (Reprint of Van Regteren Altena (1938) above) Van Regteren Altena. Mey (1989). personnel during Kendeng zone mapping survey (Duyfjes et al. Ed. p. Triphoridae. Kadar. Indonesian Petroleum Association (IPA) Field Trip Guidebook. 5. Troelstra (1981). sandstones. Mededelingen 12. p. (Late Miocene-Pleistocene planktonic foram biostratigraphy of deep water deposits of Kendeng zone in Ngawi section. (online at: www. L.J. ('The significance and occurrence of phosphate on Java'.R. Part.47. E Java. Small phosphate deposits found at many localities on Java. C.The marine Mollusca of the Kendeng Beds (East Java). J. 1-29. 89-120. Molluscs mainly from Pucangan Fm. (1926).C. Material collected by Geological Survey. 2. 1-67. most of it probably draining North. D. Early description of classic JiwoSouthern Mountains successions N of Gunung Pendoel Miocene andesite intrusion (not much different from Verbeek and Fennema 1996): Pretertiary chlorite schists and crystalline limestones. Soenarto. overlain by Eocene conglomerates (mainly quartz pebbles). p.nl/document/549625) (Systematic study of marine molluscs from Plio-Pleistocene Kendeng beds of E Java. C Java) Van Es. Budianto Toha et al. (online at: www. Fourth Pacific Science Congress.Central Java Fieldtrip 27-30 October 1989. (1938).Central Java Fieldtrip June 18-21. J.vangorselslist. Calyptraeidae.O.O.. Brief review of small mining exploration/ exploitation concessions S of Madiun.naturalis.De beteekenis en het voorkomen van fosfaat op Java. (= Lower Tf.T. Possibly 2000m of erosion prior to deposition of M-L Miocene limestone. Excursion Guide E5. D. 6.) and by Cosijn. claystones and limestones with Nummulites. Xenophoridae. 205-210. (1987). Marine Micropaleontology 6. (2) Kali Teloe (1908. Pellatispira. Indonesian Petroleum Association (IPA) Field Trip Guidebook. L..Late Neogene planktonic foraminiferal biostratigraphy and climatostratigraphy of the Solo River section (Java. Strombidae. Dienst Mijnbouw. J. (1929). part IV (Families Cassididae-Ficidae inclusive). C.. Gastropoda. p.O.J.com Sept 2016 . Leidsche Geol. Amaltheidae.('Geological observations on Java 1: Jiwo and Southern Mountains'. Epitoniidae.C. 1. N and W of Tegalombo (copper)) Van Es. Leidsche Geol. p. I (Families Fissurellidae-Vermetidae inclusive). Pyramidellidae. & S. All formations unconformably overlain by near-horizontal 'young-Miocene' limestones with Lepidocyclina rutteni.Trinil. p. all in present or former cave deposits. and Naticidae) Van Regteren Altena. etc.0 158 www. p.repository. (1935). HvG). p. Mining concessions: (1) Kesihan (19081925) S of Tegalombo (copper.T. p. Potamididae.H.J. (1943). Miogypsina. Mededelingen 10. Bandung. 217-320. C. 1-14. Eulimidae. Leidsche Geol. Wetenschappelijke Mededeelingen 27. De Mijningenieur 7. C. some Upper Kalibeng Fm) Van Regteren Altena. Indonesia). Enkele aanteekeningen omtrent het Zuidergebergte (G. orbitoiden en alveolinen in Java en over den ouderdom der gesteenten waarin zij optreden. (1883). East Java. 205-240. p. 6. Assilina. & J. Garut. Relatively high T (216-320 °C) and salinity 2-5 wt% NaCl at formation) Verbeek. Musgrove.html?id=uFoYAAAAYAAJ) ('Preliminary note on Nummulites. (1932). 5 of which have Eocene sediments unconformably overlying Pretertiary metamorphics. ('On the thickness of the Tertiary deposits on Java'. (IPA). Indonesia: a case study from the Jambaran Field.0 159 www. Zeiza. & C.Eine Neogene Molluskenfauna vom Tji Gugur (Priangan). Geographic-geological observations in Southern Mountains (Gunung Kidul) SE of Yogyakarta) Vanessa. 7. 1.. Conv. Jakarta. Tall gas column in steep-flanked Oligocene carbonate buildup with ~1000 m of relief relative to platform. C. (1950). Stephens. Akademie Wetenschappen. R. Verhandelingen Kon.com/books/about/Natuurkundig_tijdschrift_voor_Nederlands. 23.naturalis. Includes first descriptions of Eocene Nummulites (Nummulites javanus. 1-9. A. Batavia. part V (Families Muricidae-Volemidae inclusive). Verdiansyah (2014).The marine Mollusca of the Kendeng beds. Verhandelingen Kon. Ed.com Sept 2016 . ('The Jampang-Kulon District'. (IAGI). East Java (part III of this series is by Schilder 1941)) Van Regteren Altena.(www. (Rich Neogene mollusc faunas from Priangan. 132-134. 43rd Ann. N. Garut.O. 5p. C Java (smaller species than those known from W Kalimantan)) Bibliography of Indonesia Geology. J.geological observations in SW Java) Van Valkenburg. Amsterdam. High sulfidation epithermal gold deposits in volcanic rocks of Miocene Jampang Fm. S. Gastropoda. Proc. Assoc. 2.D. Sekti.nl/document/549261) (More taxonomic descriptions of Plio-Pleistocene gastropods of East Java) Van Regteren Altena. bagelensis. S.M. IPA11-G-205.naturalis.Chattian sea level fluctuations. W. Leidsche Geol. West Java'. S.O. PIT IAGI 2014-256. Jawa Barat. Conv. Geol. (Jambaran Field discovered in 2001. Batavia. NW of Jakarta)) Van Valkenburg. & O. Unconformities recognized on well logs and seismic coincide with global Rupelian. (http://books. 3-16. p. Indon. R.repository. R. (1891).vangorselslist.google. Mededelingen 15. Weidmer. Only 6 areas of Java with Early Tertiary in outcrop.T. ('Fluid inclusions in high sulfidation epithermal gold deposit Cijulang. Alveolina javana) from Java. 3767. F. Jaarboek Topographische Dienst 1924. No maps or stratigraphic context info) Van Simaeys. SW of Bandung. p. A. Petroleum Assoc. p. Geographic. Jakarta.D. p. Simo (2011)Early carbonate growth in the East Java Basin. N. orbitoids and alveolinids in Java and on the age of the rocks in which they occur'. (online at: www. p. Derewetzky & T. 13p. p.repository. Main buildup ~10 km long. Kidoel). Natuurkundig Tijdschrift Nederlandsch-Indie 51. also Timor. De Mijningenieur 13.nl/document/549495) (Taxonomic descriptions of Plio-Pleistocene gastropods of families Cassididae and Ficidae from Upper Kalibeng and Pucangan formations of Kendeng zone. White (1924). (‘On the alignment of the Thousand Islands’ (Pulau Seribu.Het district Djampang-Koelon. Geologisch Mijnbouwkundig Genootschap 14 (Gedenkboek Tesch).Voorloopig bericht over nummulieten. Nederl. 101-138. Indon.M. Beets (1944). (1924). Mention of Cretaceous larger foram Orbitolina from Luk Ulo. Jaarboek Topographische Dienst 1923. C. Java.Over de rangschikking der Duizend eilanden. A. A. Discocyclina. ('Some notes on the Southern Mountains (Gunung Kidul)'. In Cirebon area Tertiary ~5000m thick) Verbeek.Inklusi fluida pada endapan emas epitermal sulfidasi tinggi Cijulang. subaerial exposure and meteoric diagenetic events) Van Tuyn. 1 km wide. Proc.Over de dikte der Tertiaire afzettingen op Java. 35th Ann. archive. (UNPAD) 12.A.T.G. Fennema (1882). Mitteilungen 44. 173-186. Stemler. with 1:2. Amsterdam.M.M. p. (1954). (1898).D. Bogor. With beach ridges. Brief overview of the geology in German. + Atlas.org/20/items/descriptiongol11verb/descriptiongol11verb.vangorselslist. & R. R. (1953). ('Geological description of Java and Madura'. 5-48.M.Het kustgebied van Noordelijk West Java op de luchtfoto.T. J. during lowering of sea level of 5-6m. Akademie Wetenschappen.M. Doct. & R. p. Not much on geology. Nur (2014). (‘New geological discoveries on Java’.Petrologi dan petrografi satuan breksi vulkanik dan satuan tuf kasar pada Formasi Jampang. R. daerah Cimanggu dan sekitarnya. steeply dipping. Amsterdam. p. which formed in last 5000 years.ac. Natuurkundig Tijdschrift Nederlandsch-Indie 41.us. p. First to recognize Paleogene sediments and Pre-Tertiary schists in Central Java. comprehensive geologic description of Java and Madura.Die Geologie von Java. 21.Nieuwe geologische ontdekkingen op Java. 3. Yuniardi & A.M. Stemler. ('The geology of Java'. (Online at: http://openlibrary. & R. 47-90. roughly E-W strike (Junghuhn had called these Tertiary. Cimanggu and surrounding areas. s-Gravenhage. R. H. R.Geologische beschrijving van Java en Madoera. First report of Pre-tertiary rocks on Java.D. with oversized atlas of geologic maps. 1-1135.000 scale map) Verbeek. (online at: http://jurnal.R. Trio. ('Brief geological overview of Java') Verbeek. 2. p.. Geomorphical study of alluvial plain along N coast of W Java. Amsterdam. Bull.org/works/OL1558191W/Description_geologique_de_Java_et_Madoura) (or at: http://ia600508. p. 1-101. Common travertine terraces in rivers of (Pliocene?)Marl Plateau.Kort geologisch overzicht van Java. Same paper as 1881 paper above) Verbeek.Nieuwe geologische ontdekkingen op Java. Also first record of leucite-bearing volcanics of Muriah volcano. at border of Bogor and Bantam Residencies. Verhandelingen Kon. Jawa Barat. and locally great thickness of Tertiary sediments) Verbeek. p. p. in three areas: (1) metamorphic rocks of S Serayu Mts/ Lok Ulo. Y. N coast of C Java) Verbeek.pdf) ('Geological description of Java and Madura'. P. 146-152. Ed. & R.M.D. Verbeek notes similarities with Sumatra old slates). 12. p. Penggemar Alam 36. river levess. etc.D. 71. (1956).) Verstappen.250. Natuurkunde. (1897).Djakarta Bay. Fennema (1881). H. Nederlands Aardrijkskundig Gen. West Java') Verstappen. ('New geological discoveries on Java'. Rijksuniversiteit Utrecht. J.D. 37-51. Tijdschrift Kon. 25-34. R. 1-1183. Classic. Thesis.M. N of Kebumen. ('The coastal region of northern West Java on air photos'. associated with serpentinite and red chert. Fennema (1896). Afd. 2.Description geologique de Java et Madoura. (2) metamorphic rocks on three of 'Zutphen islands' in Sunda Straits and (3) Gedeh Mt near Jasinga. R.Landscape development of the Udjung Kulon Game Reserve.unpad. (Geomorphology study of poorly studied Ujung Kulon peninsula of SW Java. Nederlands Aardrijkskundig Gen.G.Verbeek.com Sept 2016 . a geomorphological study on shoreline development. 171-179. (Unpublished) Verstappen.D. which appears to be tilted to NE) Bibliography of Indonesia Geology. 2 vols. Petermanns Geogr. Fennema (1896). p.id/bsc/article/view/8378/3894) ('Petrology and petrography of volcanic breccias and coarse tuff of the Jampang Formation. H. 6. Tijdschrift Kon. French translation of Verbeek and Fennema Java book above) Verdiana. Scientific Contr.T.0 160 www. Belmont. A. E Miocene Nyalindung beds and Late Miocene Tjilanang beds in Bandung survey collections) Wachjudin. Boyce (2006). I. Aftershocks mostly in Gunung Kidul Mountains. etc. C Java. (2008). K. In upper mantle beneath volcanoes a lowvelocity anomaly inclined towards slab. Kopp et al. Descriptions of otoliths from Late Eocene of Nanggulan. collected by Selenka 1907 expedition) Vorstman. H. Martono (1985). p. 635-657.G. 739-749. Five ore/ alteration stages. Indonesia.G. Blankenhorn. Collision exhumed high-P metamorphics from deeper part of pre-existing Bibliography of Indonesia Geology. Walter. H. Williams-Jones & A.. Selenka & M. 923-932. A. Jurassic shallow marine allochthonous formation emplaced by collision of continental blocks. Jakarta. In: M. Rabbel. ('Some Neogene sea urchins from Java'. Also comments of geology of Timor. 339-352. Ed.Bericht uber einen Ausflug in Java. (130 seismographic stations onshore and off C Java and operated for >150 days. probably paths of fluids and melted materials in mantle wedge. 18. Star Publishing.2. (2000). 170. Metallogenic model explains enrichment in Sn and W by increased recycling of slab-derived sedimentary material during Pliocene subduction) Wahab. California.. Leipzig.Tertiaire vischotolieten van Java. (2007). Wagner. Kopp et al. Echinoids from Pliocene? marls in Trinil area.Application of oil geochemistry for hydrocarbon exploration in Northwest Jawa. Geological fieldtrip to W Java volcanoes and South coast by famous German geologist Von Richthofen with F.Joint inversion of active and passive seismic data in Central Java. p. (Cretaceous accretionary-collision complexes formed by accretionary or collision processes. and was likey epicenter of 2006 earthquake. Engelmann. D. p. 6. (Analysis of source rocks in NW Java shows Lower Cibulakan (Talang Akar) sediments are main source in area. p. Conv. W. 1-16. Kuhnel & S.L.. Pramumijoyo et al. Junghuhn. (eds.R. 14th Ann. siliceous shale.com Sept 2016 .J.Stable isotope-based modeling of the origin and genesis of an unusual Au-Ag-Sn-W epithermal system at Cirotan. p. 2. Int. 41-45.1.0 161 www. Inversion images show strong low-velocity anomaly (−30%) in backarc crust N of active volcanoes. p. D. S. Karnawati.Cretaceous accretionary-collision complexes in Central Indonesia. Wassermann. Applied Clay Science 5. Accretionary wedge with fragments of oceanic crust (chert. (IPA). Gesellschaft 14. 237-260. Die Pithecanthropus-Schichten auf Java. Reck (1911). In: D. one at foot of volcanic arc. back arc spreading. 2006. p. on NE-SW trending zone that separates forearc in two rigid blocks. J. Zeitschrift Deutschen Geol. S. B. Crust in forearc appears strongly heterogeneous. (1862). Koulakov. Asian Earth Sci. Distribution of mature source rocks delineated by applying Lopatin method) Wakita.vangorselslist. & H. Wittwer. pillow basalt).) The Yogyakarta Earthquake of May 27. arc volcanism. Focal strike slip mechanism consistent with orientation of this contact) Wagner. 2. limestone. Sulawesi.J. 327-356.E. Indon. T. Luehr. (1929).11.G. (Report on a trip on Java'. forearc sedimentation. p. Oceanic plate subducted under Cretaceous arc from S. Indonesia. A. W.Von Richthofen. 4.The characteristics of bentonite from the Karangnunggal deposit. West Java. carried microcontinents from Gondwanaland. A. Chemical Geology 219.A. Onshore part two high-velocity blocks separated by narrow lowvelocity anomaly. & D. van der Gaast (1990). Recent Java earthquake at lower edge of this zone. in zone semi-parallel to and 10-15 km E of Opak River fault) Wagner. Proc.Einige neogene Seeeigel von Java.Seismic structure of Central Java. Rabbel. interpreted as weakened contact zone between two rigid crustal bodies.) Von Staff. famous Java naturalist. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederlandsch-Indie 5. T. Luehr. F. J. Petroleum Assoc. H. Geophysical J. B. (Pliocene Cirotan low-sulphidation epithermal gold deposit in W Java complex polymetallic assemblages and progressive enrichment in Sn-W and Au-Ag in late stages of mineralization. ('Tertiary fish otoliths from Java'. R. p. (C Java tomographic data reveals two low velocity anomalies. Java.0 162 www. Ebinger (2008). Formed in Pliocene (2. und seine Epoke aus dem Altmiocaen der Insel Madura. H. and its…from the Early Miocene of Madura Island'.W. Ed. More than nine subparallel quartz-adularia-carbonate veins. Katacycloclypeus (= more likely Middle Miocene?.argillaceous rocks were deposited throughout Cretaceous time.Cretaceous radiolarians from the Luk-Ulo Melange complex in the Karangsambung area.Late Cretaceous (Late CampanianMaastrichtian). Atkinson (1983). P. (2006).05 Ma).E. Soc. Munasri & B.D. p. Density contrast between arc and underlying crust required to produce arc basins means they are unlikely to form in young intra-oceanic arcs) Wanner.vangorselslist. p. p. J. (’Miocene molluscs from the Rembang area (Java)’. Draut. Scholl (eds.early Late Cretaceous. Media Teknik 28.Nature and age of sedimentary rocks of the Luk-Ulo melange complex in the Karangsambung area. p. Good fit of model to Halmahera Arc and E Java. Richest mollusc localities on Dermawu-Mahindu and Gegunung anticlines. Late Cretaceous age of radiolarite above pillow basalt at ) Wakita. Eavis & T. eulepidinid Lepidocyclina. Ngandong and Lodan). Central Java. D. Indonesia.Middle Cretaceous (Barremian-Albian?). Spec. Geol. if plate is broken. Geol. Survey (USGS) Prof. 64-79. J.J. Molluscs mainly gastropods. D21-D23.Basin formation by volcanic arc loading. New crinoid species from blue-grey marls. Bambang (1991). A. Paper 436. Molluscs from area N and NNW of Bojonegoro (Sedan. 9. (On caves in C Java Southern Mountains M Miocene Wonosari Limestone) Waltham. (1938). LIPI.R. Mainly from M Miocene orbitoid-Cycloclypeus Lst (later called OK Limestone and Ngrayong Beds) and some from overlying Globigerina Marls series (later subdivided into Wonocolo. Southeast Asian Earth Sci. (Brief review and map of folded Miocene clastic sediments with andesitic intrusions at Jatiluhur damsite. Smart. Paper 450-D. Zeitschrift Deutschen Geol. M. Bogor zone. Smyth & C.. Beilage Band 79 B.Geology of Djatiluhur damsite and vicinity. Central Java. & E.M Campanian) and V. 29-43. Wanner notes N to S facies changes. half of them new) Warmada.Balanocrinus sundaicus n.Miocaene Mollusken aus der Landschaft Rembang (Java). Cave Science 10. ('Balanocrinus sundaicus n..sp. Associated with Miogypsina thecidaeformis.com Sept 2016 . p..W. and accreted at subduction trench in M.The caves of Gunung Sewu. 68 species. (Pongkor epithermal gold-silver deposit in W Java largest low-sulfidation deposit on Java. Proc. Ledok and Globigerina Marls Fms. 11-26. 222-273.C.accretionary wedge.L. Yogyakarta. J.) Formation and applications of the sedimentary secord in arc collision zones. II.. 55-96. P. IV. H.C. Jawa Barat. 385-403. Loads generated by arc sufficient to account for subsidence in basins within ~100 km of active volcanoes at subduction plate boundaries. I. Geol. Munasri & W. Gesellschaft 87.Late Cretaceous or earliest Paleocene. Cretaceous tectonic units rearranged by Cenozoic thrusting and lateral faulting during successive collision of continental blocks and rotation of continental blocks in Indonesian region) Wakita. Clift & D. Siliceous. (Incl. K. Friederich. Basins will be asymmetrical with coarse volcaniclastic material close to arcand volcaniclastic turbidites farther away. (Five assemblages of Cretaceous radiolarians in shale and chert of Luk-Ulo Melange in Karangsambung area: I. Indonesia.. America (GSA). Palaont. Neues Jahrbuch Mineral.H.sp. p. K. R. HvG)) Wanner. W Java) Waltham. 4. III. H. 4. West Java. (1962). (Paper quantifies flexural subsidence from loading by volcanic arc. Hahn (1935). p.Late Cretaceous (Coniacian. Fragmentation and mixing with schist and quartz porphyry must have occurred in Paleocene) Waldron. A. Ngampel. Hall. northern C Madura. Silver Jubilee Symposium on Dynamics of subduction and its products. In: A. Butak. Widoyoko (1994). kotoi. Formation T ~220°C) Bibliography of Indonesia Geology. p.S.Karakteristik mineralogi dan proses pengendapan emas pada endapan emas-perak epitermal Gunung Pongkor. 6. Indonesia.). collected by Weber near Bawarukem River. 32-36. U.Early Cretaceous ('up to Barremian'). carbonates. Carbonate deposition on buildups progressively terminated through time fromW to E) Bibliography of Indonesia Geology. Jakarta.com Sept 2016 .Petrology and geochemistry of intrusive rocks from Selogiri area.Geologi dan fasies batuan metamorf daerah Jiwo Barat. Sudarno & D. Central Java. I.. and short period of hydrothermal activities but did not create economic ore deposit) Warmada. p.W. serpentinite and amphibolite Intrusive rocks mainly diabase dikes. Petroleum Assoc. ('Geology and facies of metamorphic rocks in the West Jiwo area. Lehmann.Warmada.T. (Pongkor gold. Selogiri deposit formed during one or two intrusion periods.5. Bayat area with metamorphic rock outcrops. Symp. L.K. Watanabe (2006). Bayat. Resource Geology 57.7 Ma (microdiorite.silver deposit near Bayah. Spec. A. 549559. is largest low-sulfidation epithermal metal deposit in Indonesia. I. Five high-relief carbonate buildups drilled in Cepu area of E Java: Sukowati. C Java'. Nine major subparallel quartz-'adularia'-carbonate veins with low sulfide content) Warmada.N. Thick Miocene section. Proc. G. Interpreted protolith of metamorphic rocks was melange. Proc. 124-135. Conv. Derewetzky. Cendana and Kedung Tuban. Indonesia. B.T. Simandjuntak & H.. SEED-Net Symposium on Geo-Hazard and Earth Resources Management. Sinomiya. light paraffinic oil from Upper Rembang and Lower Wonocolo sands in Ledok and nearby fields. Weeks (ed. Lehmann & M.G. I. Klaten. p. The Canadian Mineralogist 41. Wijonarko (2008). 2.W.W. J. Bayat. Jogmec) and ~12. Media Teknik (UGM) 30. 113-118. probable E Oligocene carbonate platform. and is of Late Pliocene age (2 Ma). schist. rare-earth element and stable isotope study of carbonate minerals from the Pongkor epithermal gold-silver deposit. Indonesia. Soe. Indon. B. 163-169. (Selogiri gold prospect near Wonogiri in S C Java S Mountains probably formed during single intrusion periods from calc-alkaline intrusive and is not economic. Intrusions dated as ~21. Simandjuntak (2003).. Petrol.D. Banyu Urip. p. peliticrocks. Imai & K.M. C Java. 2nd Int. Liu. Hohensee. overprinted by low sulfidation epithermal gold quartz deposits. Jawa Tengah. (2) rel. Ages of intrusives Early Miocene and Late Miocene) Warmada. Setijadji. 1359-1364. Publ.Polymetallic sulfides and sulfosalts of the Pongkor epithermal gold-silver deposit.and quartz sandstones) Weeda. West Java. 2nd Int. HvG) Strontium isotope dating program. I. M.11. and (3) heavy paraffinic oil in M Mocene Ngrayong sst at Kawengan) White. expected to be porphyry copper gold deposit.0 163 www. ~N-S trending quartz -adularia -carbonate veins with low sulfide content. Geol. American Assoc.vangorselslist. In: L. (In E-W trending E Java Tertiary basin 132 MBO produced since 1888 from 20 fields. broad. gneiss and metasandstone widespread. Setijadji. Three oil types: (1) asphaltic oil from shallow Lidah and Kruka fields S of Surabaya from Pliocene U Globigerina Fm. Sinomiya. A. L. Jambaran. 2.05 Ma) and largest low-sulfidation epithermal precious-metal deposit in Indonesia.W. Soe. 185-200. (1958).C. Gross differences despite having all grown from a common. J. Watanabe (2005). (Selogiri gold prospect in W part of S Mountains. J. Timing of deposition of buildups established through robust (turns out to include bad dates.. Central Java. p. M. (Pongkor gold-silver deposit Pliocene age (2. A. E. Ed. HvG). Earth Resources Engineering and Geological Engineering Education. (AAPG). Imai & K. West Java. J. C. I.163-169. Indonesia: examples from the Cepu area. p. p. Hemes (2007). folded into 2 E-W trending zones in Plio-Pleistocene. 18. 31st Ann. A. Indonesia.. (IPA). p. Bulk of oil produced from M Miocene Ngrayong Sst (this was before Cepu oilfield discovery in Oligo-Miocene Kujung Fm Limestone.W. Three main metamorphic facies: greenschist.D. Stevens (2007). Geary.C. SW Java.V. blueschist with transition to glaucophane greenschist and amphibolite facies. V.Petrology and geochemistry of intrusive rocks from Selogiri area. intruded by igneousrocks: phyllite. Proc.Fluid inclusion. Indonesia. composed of mafic/ultramaficrocks. locally also glaucophane schist. Pierce & J. Nine subparallel.S. M.9 Ma.. 6.Oil basins of East Java. Fluid inclusions indicate temperatures of 180-220°C and meteoric water origin) Warmada. Bangkok 2005.Temporal controls and resulting variations in Oligo-Miocene carbonates from the East Java Basin.) Habitat of oil. I. Johnstone. Conv. 6p.The structural geology at Lusi mud volcano. Enschede.A. Not much detail on sample localities or stratigraphic succession) Widarmayana. (2006). 1-968.Banyu Urip and other Cepu Block fields. shallow water carbonate on horst blocks and deeper water carbonate in graben areas. Hadisaputro (2011). Prasetyo.Spatial data analysis and integration for regional-scale geothermal prospectivity mapping. 'mid-Main') coral reefal buildups along W-E trend in S part of basin.nl/library/papers_2006/msc/ereg/wibowo. D.Neogene planktonic foraminifera from Kawengan. Rapid deposition of thick organic rich sediment as part of Brantas delta. Jakarta.com Sept 2016 . Ed. E. marking transition from oblique subduction along Sumatra to nearperpendicular subduction along Java. A.Constraints on upper mantle structure and seismicity beneath the Sunda Strait from teleseismic data. B. Conv. 1-19.W..B. Sidoardjo.. Seismic tomography and seismicity pattern under Krakatau suggest (1) mantle plume ascending toward Krakatau volcano. West Java.. Santoso. (Cepu Block early carbonate growth in Rupelian in two main depositional environments. Mineral Res. Publ. Indonesia. 5p. Proc.0 164 www. Porong District. Reef sizes between 4. Musgrove (2014). Inst. at E end of Kendeng Zone in S part of E Java inverted back-arc basin formed in Oligocene. Proc. B.. Brief review Nannofossils from 26 samples of Eocene. & H. p. 32nd Ann. p. T. (Sunda Strait area of active extension. IPA14-G-336.X. 185-194.Whitten. E Java. I. Syukur. A. 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Pelitic basement deformed in Cretaceous accretionary prism and uplifted/ peneplained in E Tertiary. p. P.Dorobek S. Proc.Evolution of Cenozoic inversion structures. R. J. N of Ujung Pangkah Fld also E-W trending left lateral strike-slip movement) Ebanks. AAPG Ann. M.G. 197-223.A. Ph. Basin-bounding faults listric and inferred to sole into sub-horizontal detachment at <10 Bibliography of Indonesia Geology.O. Underlying crust transitional between Sunda craton continental crust to W and Banda back-arc oceanic crust to E. Conv. Suchecki & S. & A.J. Indon.D.E Oligocene.P.vangorselslist.Geological reservoir heterogeneity of Talang Akar depositional system in the Jatibarang Sub-Basin.. farther apart. 35th Ann. Extension and regional subsidence continued until E Miocene. p. IPA Core Workshop Notes. Indonesia.. Leeward (E) margins of W-most platforms greatest amounts of progradation and filling of interplatform troughs. W.0 177 www. Atkinson et al. p. 6. A. K. Young (1972).Conditions conducive to coalescence of isolated platforms in the Miocene Wonocolo Formation. In: C. (1996). Uktolseja & E. E. Smaller platforms in E part of study area steeper sided.) Clastic rocks and reservoirs of Indonesia. Thesis Rice University.W. Sunderland. North Madura area. ENE. Paleogene extensional faulting may have lasted throug Kujung Fm deposition.trending half-grabens formed in Sunda back-arc in M Eocene. Indon. H. etc. 2. Ed. In W part of area individual platforms larger in plan view than age-equivalent platforms to E and show initial development of several closely spaced isolated platforms that coalesce at middle of growth history into larger composite platforms.Cenozoic inversion structures in a back-arc setting. Cook (1993). possibly due to faster subsidence rates in E) Dorojatun. Penetrated ~320' of Banuwati Clastics member that overlies granitic basement. with average porosity of 13. Bibliography of Indonesia Geology.com Sept 2016 . In: Proc. including lacustrine coals. Conv.Structure and stratigraphy of AVS Field.. R. horizons defining growth phases of inversion structures correlate with eustatically-controlled unconformities on basin margins) Emmet. presumably Australian margin. Recoverable reserves >20 MBO) Faisal. Expl.0 178 www. E-W orientation of better imaged keels may represent fabric of source terrane. (AVS Field multiple Oligocene Talang Akar Fm channel sand reservoirs. Howes (eds. In: C. Proc. Indon. Fainstein. Gas habitats of SE Asia and Australasia. 15th Ann. Indon. (Deeper play in Asri basin tested in 1995 Hariet-2 well.. Proc.A. offshore NW Java.E Miocene regional sag with aggradation of shallow water carbonates on basin margins. Surabaya 2005. Ed.A. 1. P.C. Vail (1996). No communication between multiple reservoir zones. Paleogene extensional basins progressively inverted as thick wedges of Miocene and younger calcareous mudstone accumulated on flanks. (2005). East Java Sea. Proc.R. J. Joint Conv.G. Twenty oil. Proc. Indon.bearing reservoirs.) Fainstein. (Abstract only. & L Suffendy (1999). & Munji S.W. Int. Granath & M. 169-178. (E Java Sea deep seismic imaged up to 5 km of pre-M Eocene beds below angular unconformity. S8. (IPA).V. 58th Ann. Most inversions trend ENE and grew in bathyal water depth. These 'synformal keels' lie below known inversion structures. 1. R. South East Sumatra. Jakarta 1998. Conv.A.A. uplifted and truncated in latest Miocene. Extensional structures controlled by pre-existing thrusts and shaly bedding planes in basement.Deep reservoir challenge in Asri Basin. Inversion progressed through Miocene and culminated in development of regional basement-involved inversion high (E extension of Kangean high). 6. p. R. Conv.Seismic exploration of the Thousand Islands area. p.. Petroleum Assoc. Mtg Soc.vangorselslist. indicating Eocene extensional basins and Miocene inversions nucleated on pre-existing structures. Geoph. but widespread secondary moldic porosity) Fisher. Anaheim.6%. 14th PERHAPI. In Miocene N margin of basin strongly progradational reflecting tectonic stability and dominant eustatic influence. Conv. & P. p. IPA09-G-046.8 mD. Northwest Java Sea.) Proc. Dinkelman (2009). (1987). Inversion began in E Miocene as basin-bounding faults reactivated and graben-fill sediments displaced towards adjacent horst blocks. & V. locally preserved in faulted synclines 20-50 km wide. Eocene rifting in few deep basins. p. P. Oil is on structural roll-overs confined laterally by growth faults of Thousand Islands Fault System. Late Oligocene. Despite regional compression which continues today at deep structural level. deep-water carbonate mudstone and shale in basin axes. Java Sea. 34th IAGI.Pre-Tertiary sedimentary “keels” provide insights into tectonic assembly of basement terranes and present-day petroleum systems of the East Java Sea. Jakarta. Jakarta. Fainstein. S margin back-stepped due to higher tectonic subsidence related to inversion process. Indonesia: can tectonic and eustatic influences on stratal architecture be distinguished? AAPG Ann. (IPA). Two facies (1) fluvial/upper deltaic and (2) transitional/lower deltaic. Java Sea. Caughey & J. (IPA). Petroleum Assoc. transgressed by Late Eocene shallow-water carbonates on margins of rift basins with shale dominant in basin axes. Conf. 11p. 16th Ann.km. Bintoro W. 30th HAGI. Sandstone heavily compacted. 19-45. permeability 10. Indon.Cenozoic inversion structures.. In deep basin. Pramono (1986). Oligocene rifting more broadly distributed in shallower basins.R. 877-881. p.Exploration of the North Seribu Area.Dim spots and non-bright AVO associated with gas in the South Arjuna Basin. D.7. Checka (1988). Petroleum Assoc. San Diego 1996. Onset of compression in E Miocene reflected by increase in subsidence and sedimentation rates. small-displacement domino-style normal faults ubiquitous at shallow structural level and apparently form on flanks of growing inversions by gravity sliding) Emmet. 191-214. 33rd Ann. R. Petroleum Assoc. SEG. penetrating Eo-Oligocene oil sandstone below 310' thick Banuwati Shale lacustrine source rock. & H. Extensional half-grabens in Sunda back-arc filled by M Eocene non-marine siliciclastics. SE Sumatra.Fletcher. Int. while south correlates to Australian craton) Granath. 1-16. & P. Jakarta 1995. 1. In: R.E Paleogene overlap assemblage.. p. Banda Sea.vangorselslist. likely formed during repetitive sea-level lowstands in Pleistocene. (IPA). p.. T. 4th Ann. offshore Northwest Java. 33rd Ann. Dinkelman (2009). Asia.K. Conv. Original oil-in-place 98.W. (eds. and Neogene inversion.G.0 179 www. 14th Ann. (Unpublished) Gresko. IPA09-G-047. Petroleum Assoc. Bay (1975). IPA10-G-007. Caughey et al. West Madura Block. Conv. p.Talang Akar coals.A.Sc. J. p. Indon. Jakarta. G. 20-30km wide. (IPA). J. 34th Ann. J. Dinkelman (2010).G. P. Located within large erosional valley.A. Suhana & I. Soc. & K. Jakarta. E Java Terrane rifted from NW Australia in Jurassic and accreted onto magmatic arc of SE Kalimantan in Cretaceous) Granath. 91-120. 14p. (1980).L. Indon.) The SE Asian gateway: history and tectonics of Australia-Asia collision.Pre-Tertiary of the East Java Sea revisited: a stronger link to Australia. Sequence Stratigraphy in S.M. 13p. (1985). Jakarta.Pre-Tertiary sedimentary section and structure as reflected in the JavaSPAN crustal-scale PSDM seismic survey. (IPA). A.Neogene clastics and carbonates representing Paleogene extension. 6.5 MMB Oil and 292 BCF gas.Upper Eocene-Lower Miocene planktonic foraminiferal biostratigraphy of wells JS 25-1 and JS 52-1. Suggest departure of E Java Terrane from Australian margin in Late Jurassic and suturing to SE Sundaland in mid-Cretaceous. Jakarta. J. P. Asjhari (2005). p.A. Indon. 2. In: C. 1-112. cratonic sedimentation and inversion similar to Goulburn Graben of Arafura Shelf. (New regional seismic survey in Java Sea and Makassar Strait suggests E Java Sea underlain by continental basement with prolonged multiphase history of deposition punctuated by extensional and compressional events.) Proc. Publ. Christ. From there fluvial systems drained into Indian Ocean through Sunda Straits) Bibliography of Indonesia Geology. W. (Identification of incised-valley complex on 3D seismic. Proc.5 km thick on basement in number of fault blocks. Proc. N part of EJT (affected by Eocene Makassar Straits extension) probably related to E Indonesian islands and Tasman orogenic belt. Indonesia.W. (Seismic lines over Pre-Tertiary in E Java Sea area suggests history of rift-fill.. 21-33.G. Sukmana. Emmet & M. (IPA). (eds.M. Indonesia. producing oil from 1975-1978 the again since 1998. E Java Terrane is major part of SE Sundaland between Meratus suture.A. SPE 93137. (East Java Sea-Makassar Straits. Precambrian-Permo-Triassic sedimentary section (age assumed) up to 8. Emmet & M. Kujung-I oil reservoir.W.Seismic expression and channel morphology of a Recent incised-valley complex. Ed. 355. Indon. 2001)) Gordon.W. NW Java Basin. Conv. Lowry (1996).K. unconformably overlain by thin Cretaceous. 211-240. (IPA).J. M. 53-74.com Sept 2016 . >300 km long and >100 m relief.Ardjuna subbasin oil source.Y. Conv. Thin oil column below large gas cap (see also Welker-Haddock et al. Spec. Java arc and W Sulawesi orogenic belt. It focused drainage from fluvial systems in NW Java. Jakarta 2005. Petroleum Assoc. and its implications regarding the basement terranes in the East Java Sea. and possibly S Borneo into area of present-day Java Sea. M. suggesting main source rocks are in U Cibulakan and Talang Akar Fms) Forrest. Flores (oceanic) basin deep seismic lines) Graetzer. Christ. East Java Basin. (Early ARCO source rock paper. Hall et al.Reservoir simulation challenges for modeling an oil rim with large gas cap in the Poleng Field. (On reservoir simulation model for Poleng field ~30km off N coast of Madura. but is poorly constrained in N under N Makassar Basin and in Kalimantan. Dinkelman (2011).Crustal architecture of the East Java Sea-Makassar Strait region from long-offset crustal-scale 2D seismic reflection imaging. from Miocene Kujung Fm carbonates. Proc. Geol. Emmet & M. unconformably overlain by M Eocene. In: SPE Asia Pacific Oil and Gas Conf. M. Petroleum Assoc. J. Thesis University of Oklahoma.. Symp. Indon. Petroleum Assoc. London. Offshore Eastern Java. Petroleum Assoc.L.E. J.Geochemical evaluation. sag. p. P. Proc. (One of first papers to propose coals as oil source rocks in fields off NW Java) Granath. IPA10-G-072. Hafsari. Int. 6. the Oligocene Talang Akar Fm) Guntoro. 29-41.the Kujung Formation revisited. Indon. Underthrusting plate may extend to negative gravity anomalies of Flores Island. Indon. Proc. B. Harris. Supardi. (1992). Conf. Mesdag. or gravitational instability is pulling it down into asthenosphere. 1-13. 6. Large sag basin over three precursor rift halfgrabens. Ratanasthien & S. Wetar N of Wetar-Alor and Flores thrust N of Flores-Sumbawa. B. Indon. High basement blocks on margins sites for thin clastic deposits and thick shallow water carbonate buildups. with series of sediment filled. Kangean Block. affected by deep marine platform diagenesis and shallow marine platform diagenesis. (Late Eocene extension led to formation of E-W trending rift system in Kangean Block. 34 th Ann.E. S.vangorselslist.Integrated 3-D Static reservoir modeling of Upper Pliocene Paciran carbonate in the Sirasun gas field. Petroleum Assoc. Jakarta. p. In: B. Choiriah (2003). (IPA). S.East Java. (2003). 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Large negative free-air anomalies over accreted wedge 30 km S of deepest part of the Flores Sea suggest underthrusting plate is pulled down. offshore southeast Sumatra. important for development of fracture porosity. Shallow marine platform affected by marine diagenesis. 1-6. RD PSC. Chiang Mai. Late Miocene structural inversion overprinted earlier extensional fabric. After burial to 12. an indication of a new subduction reversal polarity in eastern Indonesia. M.com Sept 2016 . (1999). 148-161. & S. East Java Sea. Choiriah (2002). Alkatiri. with varying amounts of primary hydrocarbon source rocks and reservoir facies.U. Ed. p. p. Conv. Kangean PSC East Java Sea. Surabaya. Proc 29th Ann. Sinclair (1995). SEAPEX Press 4.Oligocene rifting event.Tectono-stratigraphy of a Late Eocene rift system within the Kangean PSC Block-East Java Sea. & S. Asymetric half-graben axes sites for Ngimbang Clastics source and reservoir facies and deepwater Ngimbang Carbonate facies. (Ardjuna Basin on S edge of Sunda craton. (IPA). Offshore Northwest Java. (IAGI). Conv. Van Eykenhof et al. Geol. p. (Eocene Ngimbang Carbonate buildup in core from RD 3 well. Sydney 1992. L.. S. 12p.000'. meteoric subaerial exposure and burial diagenesis. 31st Ann.8%) and permeability (0. >99% methane) Hafsari. (E Java Sea Sirasun Field 1993 discovery with >200' gas column Upper Pliocene Mundu Fm globigerinid foraminiferal grainstones (called 'ramp-type platform facies'). 91015. (Abstract only). 16-25.U. Indonesia.L..Diagenesis and fracture development of the Eocene Ngimbang carbonate RD-3 well. Upper sequence did not develop fracture porosity because of high detrital clay content and has poor reservoir potential) Harmony. Sartika. R. Conv.L. F.1 md). East Java Basin. W of Kangean Island. Indonesia. N. A.W. D. Indonesia.Characteristics of the lithofacies and depositional environment of the Eocene Ngimbang. (Brief review of Kujung Fm Oligocene-Miocene carbonate play and recent hydrocarbon discoveries) Henk. as in subduction zones. Ray-3 Well. Effect of subduction polarity influenced by type of basement) Hadiyanto. C. AAPG Int. Proc.0 180 www. originated during Eocene. P. Deliani & O. M. Search and Discovery Art. Indon. (IPA). facing and non-facing half-grabens. 389-402.W. F. 32nd IAGI and 28nd HAGI Ann.Basin evolution of the Ardjuna rift system and its implications for hydrocarbon exploration. Takano (2010). Symp. Petroleum Assoc. 24th Ann. (2003). p. 1. Jakarta.) Kaldi. Kujung I and II/III carbonates extensively karsted. Northwest Java. mostly flowing from N to S.B. (IPA). Mtg. 2005. Source rock in up to 6 km deep kitchen in SE. Central part of N Madura Platform Kujung I buildups up to 150-250 m high tens of km2 in size. (MB field MMC build-up. Whitaker (2008).New insight into the petroleum system in the East Java. Nusatriyo & C. Situmorang (1994). Three trends (1) S Makassar-Central Deep area. Result of study is retrograding carbonate build-up model) Johansen. 99-117. Proc. 373-393.B. 10p. Build-ups encased in mostly non-permeable sequences. low relief inversion anticlines.. Geologi Sumberdaya Mineral 4. 17th Ann. 1. (IPA). 2003. Geol. J. Jakarta. separated by lagoonal facies. when Java Sea was exposed land area. Inversion several phases through M/U Miocene. Jakarta. Structures in Kujung II/III large. similar to Bukit Tua and Jenggolo fields. D. Delta plain shales and pro-delta shales poor seals due to limited seal capacity (delta plain) or too thin (pro-delta shales)) Bibliography of Indonesia Geology. 1-7. H.S. so carrier beds in Ngimbang or Kujung Fm critical. A. Honda & H. mixed lacustrine. Ilahude. & M. 137-162. Proc.Seismic reflection study on paleodrainage pattern of the Sunda River. Jawa Sea. (2) Sakala-Lombok Ridge. 6. (Numerous prospects along N Madura Platform in Kujung I and II/III carbonates. main faults NE-SW. (Back-arc extension in Paleocene-Eocene formed basins around SE part Eurasian Plate. H. Kujung I play combined stratigraphic/ structural.A. (Study of Pleistocene paleochannels in area near Masalembo. K. In BZZ area best seal delta front shales: high seal capacity. p. p. (Seal potential comprises 1) seal capacity.G.Forward sediment modeling of carbonate platform growth and demise. offshore NW Java. Indon. U. Y.Kujung Fms). East Java basin: example North Madura. T. (in Japanese) (Abstract only). but 'thief-beds' potential risk. (2005). Conv. Simo. (3) offshore SW Sulawesi overall NW-SE fault trends. but proven by discoveries along N Madura Platform) Johansen. Hutapea. Several transgressive-regressive cycles in overal transgressive succession. Sutanto (2010). Proc.Seal potential of the Talang Akar Formation. Kujung II/III carbonates different facies in stable carbonate platform area. J. Nishita.. T. 17 p. Indon. with 3-4 km potentially mature source rocks. Petroleum Assoc. Eocene clastics and potential Late Oligocene carbonate plays in S Makassar. K. Karst breccia facies also recognized. probably extensions of SE Kalimantan drainage.Hughes. formed during several build-up development stages. BZZ area. Petroleum Assoc. Long distance migration main risk. but brittle and prone to fracturing.H. Indon.M.The K-39 reservoir characterization for simulation. EUR ~34 MBO.The dynamic of hydrocarbon migration and accumulation around Kangean Island. Ann. Indonesia. deltaic and marginal marine sediments (Ngimbang. Japanese Assoc. Proc.Present. Proc. as revealed by 3D and 2D seismic data.Depositional model of the MB Field Mid-Main carbonate reservoir Offshore Northwest Java. Important inversion phase. S Makassar Basin little affected by inversion. initiated in E Miocene. Saefulah & T.vangorselslist. Assoc. faults mainly E-W. 2) seal geometry and 3) seal integrity. etc. Indonesia. and merging with W to E orientated channel ('South Sunda River') in S of study area) Isworo. Conv. Ann. Conv.com Sept 2016 . Ardjuna basin. Proc. particularly along Madura/Kangean wrench zone. probably several phases of exposure. offshore.A. (IAGI). Ruf & F. Petroleum Technology. Older extensional faults reactivated and some Eocene basins inverted. Ichimaru. Proc. (IPA). Large number of leads: Ngimbang carbonate and clastic plays over Lombok Sub Basin. Three channel types (horizons). p. thick. Petroleum Assoc. Potential is moderate in upper TAF transgressive carbonates: high seal capacity and continuous. East Java. 32nd Ann. Most traps 10-50 km from mature source.D. 2010. 27th Ann. Atkinson (1993).South Makassar Area. Viable source rock main challenge in area. Indonesia. Conv. Indon. is N-S elongated patch reef complex. J. E. 22nd Ann. SEAPEX Conf. Ed. Prasetyo (1999). (IPA). 29. & C. Conv. Petroleum Assoc.. Wu (1988). Indon. laterally continuous and very ductile. off Southeast Kalimantan around Masalembo waters.S.0 181 www. 2-10. Jakarta.Depositional geometries and hydrocarbon potential within Kujung carbonates along the North Madura Platform. p. producing since 1994 from fluvial M-U Eocene Ngimbang Clastics Fm) Liu. p. Ed. this charge of gas flushed preexisting oil accumulations. 177-192) (Reservoir description for Pagerungan gas field.. Secondary porosity and fracturing produced good reservoirs) Kovacs. but actual gas column is 328 m) Kaldi. 43. p.D.L. with reefs as exploration targets. Techn. Beijing.Seismic expression of Late Eocene carbonate build-up features in the JS-25 and P. Proc. Jakarta.N. Jakarta. X. 120. p. O'Donnell (1997). Noble (eds. breached traps refilled with gas over periods as short as perhaps 2-3 My) Keijzer. (IPA). (2009). thick E Miocene limestone and shale sequence (Kujung Unit I). Australia. In: R. Features grew over basement highs. 85-101.Seal capacity in dynamic petroleum systems: example from Pagerungan gas field. C. (1982). Acta Sediment. 280-288. O’Brien & T.limestones with bioherms (Poleng Field). Offshore Northwest Java. Indon. principally gas. 5. (b) extensive.Rama reservoir model study. Kaldi.V. D. J. (Seals in E Java Basin dynamic rather than absolute barriers to fluid flow.) Seals. Paper 35611.Reservoir characterization constrained to welltest data: a field example. 325-334. Petroleum Assoc. R. Data from largest gas field. p. Geol. Conv. Indon. P.. Main E Miocene physiographic elements (a) deep water. Prod. p. Some uncertainty whether the Bawean volcanics pre-date or postdate Miocene limestones) Kenyon. American Assoc. Bibliography of Indonesia Geology. (1985).pdf) (Bawean island. p. 437-447. suggest dynamically filling and leaking capillary trap. & C.. Akademie Wetenschappen. Conf.C. Petroleum Assoc. Sinica. 73-86.A contribution to the geology of Bawean. Jakarta.vangorselslist. 1. p. Proc. JS25-1 well penetrated >1000’ of recrystallized Late Eocene limestone. Wang H. traps and the petroleum system. (IPA). (online at: www.nl/DL/publications/PU00017446. (Classic paper on E Java Sea. J. Nederl. Petrol. 39. 27.A. Sunda Basin. rel. A. Horne. East Java Sea.. Discovered in 1985. supports maximum gas column of 213 m.G. (1977). (AAPG). Soc.com Sept 2016 .. Howes & R. 2. Java sea. 619-629. 1. with high energy bank along S margin. Indonesia. Petroleum Assoc. East Java Sea. Petrol. whereas subsidence in new depocentres was drive for renewed hydrocarbon expulsion and migration. Denver 2000. Timor Sea Neogene tectonism caused extensional faulting and basin formation. Indonesia. Proc. J. Australian Petrol. Kon. Expl.D. p. Widespread. E Bawean Trough to W of JS-1 Ridge.JS25 area in Kangean block off N Bali. Jenkins (2000). Sepanjang trend. N of Madura Island. 67. (also in Proc. 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Deng H. with shoal water carbonates. (APPEA) J. Singapore. Conv. Engineers (SPE) Reservoir Evaluation and Engineering 3.P. (c) Central Depression with open marine. E-W trending open marine clastic basin in S (E Java-Madura Basin). (Over 20 carbonate build-ups at top Late Eocene carbonate shelf sequence. Mem. 14th Ann. Faulting caused breaching of traps. Petroleum System of South East Asia and Australasia. J.S.Kaldi. 215-238. Indonesia and the Timor Sea region. E Java Sea.Seal capacity and hydrocarbon accumulation history in dynamic petroleum systems: the East Java Basin.G.0 182 www. spreading E-W across Sepanjang island. p. Conf. Surdam (ed. Amsterdam. In: J. (Seal capacity measurements suggest Ngimbang Shale top seal over Pagerungan Field. In traps with high seal capacities. Pagerungan. Cui Yi & Di Y. Decker & W. D. Eocene-Oligocene doming and faulting followed by subsidence and tectonic quiescence until E Miocene. delta. Expl. (E Java Sea Basin metamorphic basement. 22p. Proc. 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Tertiary structural evolution mainly dip-slip fault movement during extensional and contractional phases. affecting progressively larger area with time. Regional intra-Oligocene unconformity overlain by Oligocene. Depositional systems include fan delta. Indon. (Kurnia-1well near S coast Madura island drilled rel tight (basinal?) Kujung Fm limestones. Petroleum Assoc. Ed. Petrol. Proc. but reservoir potential enhanced by fractures) Manur. coastal plain and shelf clastic and carbonate sediments. Bransden (1995). Late Miocene structures generally dry. Wrench faulting.E Pleistocene.. Continuous regional subsidence during inversion history.Structural control on hydrocarbon habitat in the Bawean area.E. 6.. locally onlapping Eocene rocks. Bibliography of Indonesia Geology. M-Late Miocene uplift in E part of basin. Indon. Great Britain Carbonate Conf. Neogene wrenching and Late Neogene compressional thrust folding. 499-510. Soc. Karst zones exhibit varying degrees of porositypermeability because of dissolution and probable fracture enhancement and flowed up to 4500 BOD at DST) Maynard. Paleogene fault zones reactivated in Neogene. E Oligocene regional subsidence. Contraction and peneplanation of Cretaceous sediments and basement before middle E Eocene produced regional unconformity. Proc. Indonesia. H. down-to-S normal faults. overlain by up to 3 km marine Upper Cretaceous sediments. Pre-Late Miocene structures more attractive targets) Matthews.The Kujung Formation in Kurnia-1: a viable fractured reservoir play in the South Madura Block. Armandita. T. (IPA). Increased permeability associated with karst confined to thin zones. (Bawean area two phases. IPA10-G-005. K. Further uplift/ N-S compression in Late Miocene-E Pliocene. IPA12-G-072. H. Ketapang PSC. Petroleum Assoc. platform carbonate. Nov. sediments dominated by deep marine clastics. fluvial. C. Indonesia. East Java Basin. Petroleum Assoc. East Java. Romi (2012). Paleogene fault-controlled sub-basins with fluvial. Conv.E Oligocene normal faulting pulses. K. Jakarta. nearshore subaqueous fans and beach) Magee. M. 317-330. 1-13. 30th Ann.. 129-144. (JS-1 Ridge in West Madura Offshore area at least three tectonic regimes: Eocene NE-trending extensionrifting. & W. Petroleum Assoc.0 183 www. lateritic clays and lacustrine shales (source rocks). E Eocene. Mandhiri.E Oligocene with transgressive marine sandstones and limestones including reefs.Structural reactivation and its implication on exploration play: case study of JS-1 Ridge. D. with good source potential. p. A.The Krisna lower Batu Raja waterflood: an updated case history. Sr ratios of most Bima samples follow normal Tertiary trend. 441-460. 21st Ann. Proc. (N Madura High E-W trending Ngimbang (M Eocene. Ramos (1998). Jakarta. Many uncertainties remain regarding distribution of facies and porosity. Indon. 559-572. (2002). J. Oil-source correlations suggest oils from center or W margin of Sunda Basin mostly from middle Talang Akar. In: Proc. American Assoc. near-basement carrier beds and Ngimbang and Kujung II/III carbonates. Pagerungan Field. IADC/SPE Drilling Conference. 5.0 184 www.. Indonesia. p. 12p. (IPA). Xu (2015). J.Application of sequence stratigraphic concepts and depositional models for reservoir mapping: an example from the Upper Cibulakan Formation in the L and LL Fields. p.G. Jakarta. Petroleum Assoc. some interpreted as NNE trending tidal ridges) McCaffrey. Jakarta. & J. Smith & S.20 km from fringing reefs. Rusmantoro. Fringing reefs viable play. 728-729. B. Jakarta.Earthquakes. with 1-6 % TOC in Talang Akar Fm. p. Payang 2001). Murtani.(Bukit Tua 2001 N Madura platform. IPA15-G-055. Dallas. Indon. Indon. M. (1985).Exploration of the North Madura platform. (late E and M Miocene Massive and Main sand reservoirs. Mursid (1992). 35th Ann. NW-SE. (Shale source rocks in Oligocene Talang Akar and E Miocene Batu Raja Fms. Petroleum Assoc. 403-430. as indicated by discoveries in Ketapang PSC (Bukit Panjang 2000. 2. Sidayu 2000). Overlying Batu Raja Fm TOC up to 3. 6. 14th Ann. Geol.Strontium isotope chronostratigraphy and diagenesis of the Batu Raja Limestone. 21. (AAPG) Bull.E Miocene) shelf edge carbonates. Proc. Migration of low 87Sr/86Sr early Tertiary marine formation waters up fault and into porous horizons likely mechanism for rock alteration) Molina. Petroleum Assoc. 1. Offshore Northwest Java. KE-24. (Abstract only) (Sr isotope chronostratigraphy from 7 Bima field wells indicates Batu Raja limestone deposition started in Late Oligocene (26-27 Ma) and ceased in E Miocene (21-22 Ma). N. 597-607. Indon. (IPA). Porosity may be from repeated exposure on crest of old Madura Platform. nearby W Madura blocks (KE-23B. (IPA). Petrol Assoc.E Oligocene) and Kujung (Late Oligocene.com Sept 2016 . 74. KE-13. offshore Northwest Java. and in overlying Kujung Fm.Petroleum geochemistry of the Sunda Basin. p.W. rich in amorphous and herbaceous kerogen. 28th Ann. KE-30) and Pangkah (Ujung Pangkah 1998. Eustatic sea level drop at ~21 Ma exposed Batu Raja carbonate platform to meteoric diagenesis and formed reservoir facies. Proc. north of Bali. E Java Sea) with three dominant fracture orientations: NE-SW. Pireno (2002). indicating generation from terrestrial and aquatic kerogen types.G. A. Proc. P. 143-179.S. D. Petroleum Assoc. Conv. produced by thrusting along Flores backarc thrust zone) McChesney. Ed. Nabelek (1987). E Java Sea. New Bukit Tua and Jenggolo oil-gas discoveries targeted layered Kujung platform carbonates on N Madura Platform. Upper Talang Akar coaly. & J. Conv.E. D. Conv. also dominated by woody-coaly organic matter. R.Seismic lineament analysis of a fractured limestone reservoir in the Ujung Pangkah Field. Eight oil families identified. Mudjiono. 2. Oil generation from lower Talang Akar started in M-L Miocene) Moulton..vangorselslist. Miller. Migration pathways via permeable Kujung I carbonates.G.E Miocene Kujung Fm carbonate reservoir in Ujung Pangkah oil field (SW part of JS-1 Ridge. p. With good basement and paleogeography maps). Petrol. (Oligocene. and E-W) Bibliography of Indonesia Geology. Zones significantly affected by early meteoric diagenesis have anomalously low ratios. 10. (IPA). Patria & J. 28th Ann.Optimizing drilling strategies in a tectonic belt. Also. Conv. IADC/SPE Paper 39357. Jakarta. offshore.. Conv.0%. M. Proc. Dwiperkasa.S. Kaldi (1990). East Java. Includes overview of regional setting) Mazied. Wilton & G. R. gravity and the origin of the Bali Basin: an example of a nascent continental fold-and-thrust belt. D. Geophysical Research 92.R. p. Indon. lower 87Sr/86Sr values in altered samples near Seribu fault. 707-722. & G. along E margin mostly from lower Talang Akar. oil and gas discovery in 300’ section of E Oligocene Ngimbang Fm/ ‘CD’ platform carbonates on basement.K. (IPA). (Bali Basin is downwarp in Sunda Shelf crust. Indonesia. midOligocene and Plio-Pleistocene. ?Holocene basalts. low-metamorphic sandstones. but laterally-restricted fluvio-deltaic deposits and thinner (~60 m). Proc.H. KBank relatively flat top with marginal banks of suspected Pleistocene origin as interpreted from seismic) Pireno.D. Proc. 13p. steeply dipping. mainly to SW (so unlikely to be part of Cretaceous accretionary terrane?. (IPA). & F. I. Ngimbang and Pre-Ngimbang at maximum burial today in syncline. 1. ~1 TCF in Plio-Pleistocene Paciran Fm sandstone and foraminiferal limestones. 301-314. offshore northeast Java Sea. HvG). (Terang-Sirasun 1982 field N of Bali >99. Roberts (1988).E. Play fairway analysis with emphasis on reservoir distribution on N Madura Platform. with N limb subcropping beneath JS 53 and Igangan-1.662. Petroleum Assoc.Source characteristics of Terang-Sirasun bacterial gas field. Coral Reefs 6.vangorselslist. 149-159. Noble & F. (eds. In: R. Darma & F. Ed. R. L46-1 well tested oil in Eocene non-marine sandstone) Bibliography of Indonesia Geology. G. Indon. H. Organic Geochem. Deepwater and Frontier exploration in Asia and Australasia Symposium. Conv. Proc. Underlying basement NE-SW trending fold-thrust belt(s) (steeply dipping reflectors to NW on 3D seismic?)) Phillips. Indonesia. 50 km E of Sunda Shelf margin in E Java Sea.A. & H.G. with top sloping from ~20 m water depth in N to ~100 m in S. 321-332.Deep-water petroleum systems of the Southern Basin. Ramsey (1972). & F. p.Ngimbang clastics play in the East Java Basin: new insight and concepts for North Madura Platform. unfossiliferous. Henk (1996).L. eastern Java Sea (Indonesia). p. Geologi Indonesia (IAGI) 2. Conv. with sedimentation starting with M Eocene lacustrine sediments.H.A.A. p. Jakarta. phyllite. conglomerate.Seismic characteristics and accretion history of Halimeda bioherms on Kalukalukuang Bank. 25th Ann. First Ann. Jakarta. 13-20. (IPA). probably always exposed during Tertiary) Nedom. Consists of thick (~90 m). possibly isoclinally folded. (Abstract only) (Terang-Sirasun gas field 100 km N of Bali in E Java Sea. steeply dipping. Structural grain NWSE. Inversion events in Late Eocene.Nayoan. K-Bank isolated limestone platform. (Southern basin is Early Tertiary NE-SW and E-W half-graben..Hydrocarbon charge of a bacterial gas field by prolonged methanogenesis: an example from the East Java Sea. Cretaceous sediments overmature and non-generative. Paleocene-M Eocene Pre-Ngimbang Fm probable gas source at Pagerungan. Noble et al. R. p. & H. (2004). Indon. Jakarta. Noble. (IPA). unconformably overlain by horizontal. Indon. but more extensive glauconitic shallow marine sandstones. Petroleum Assoc. C. Kangean Block Northern platform.H. Proc. R. 1-3.A.) Proc. Pagerungan Field produced 1. Jakarta.5 TCF gas from this play. Older formation correlated with Upper Triassic flysch by Van Bemmelen (1949). 1p. (Ngimbang Clastics is syn-rift succession in several NE-SW trending Paleogene half-grabens in E Java Basin. Two formations: Karimunjawa Fm Pre-Tertiary. p. Conv. 20th Ann. 6. 2. Indon. (Extensive areas of Halimeda bioherms on Kalukalukuang Bank (K-Bank).A. T. Indon. Hydrocarbon generation triggered by sedimentation associated with Late Miocene N-S compressional event) Phipps.Exploration and development of a new petroleum province. Jakarta. Henk (1998). 111-137.H. Indonesia. Sinartio (1991).A.J. Petroleum Assoc. Indonesia. 29.W. Gas >99% methane of microbial origin in anoxic marine setting) Noble. (IPA). and probably southernmost Sundaland. Marine incursion started in mid Late Eocene. Seismic shows E-W trending syncline in Cretaceous and PreNgimbang N of Pagerungan.0 185 www. Petroleum Assoc. 40th Ann.A.S.F. Petroleum Assoc. p. sealed by Quaternary Lidah Fm shales) Nugraha. Karimunjawa Arch surrounded by onlapping Tertiary sediments. IPA16-98-G. North Lombok. Darmawan (2016). H. (Karimunjawa Islands in Java Sea N of Semarang up to >500m elevation. 637.com Sept 2016 . (1975). (Oil in JS 53 and gas in Pagerungan from Eocene and older source rocks in E-W trending kitchen between fields. Late Eocene Ngimbang Fm coals and carbonaceous shales correlated to oil at JS 53 and condensate at Pagerungan.V.. G. S limb subcrops beneath Pagerungan.Geology of the Karimunjawa Islands.5% biogenic methane in Late Miocene-Pliocene Paciran Mb sandstone and globigerinid limestone. Java Sea. (IPA).Origin of hydrocarbons. Conv. (M Miocene Upper Cibulakan E-M Miocene ‘Massive’ and ‘Main’ hydrocarbons controlled by depositional facies (deltaic and shelfal) and mature Oligocene source rock distribution.650m wide channels normal to platform and terminate at buildup margin. Indonesia. Purnama & D. Checka. Petrol. Conv. Larger Kujung 1 patch reefs coalesced to form NW-SE trending platform. unincised. p. Expl. IAGI.) Posamentier.Lowstand alluvial bypass systems: incised vs. M. 359-373. A. characteristically sharp-edged and thicker on one side. (AAPG) Bull. Stinson (1989). Warmath. separated by 1. C.W.V.com Sept 2016 . Offshore Northwest Java Basin. Petroleum Assoc. American Assoc. Ed. up to 400m thick with diameters 1. C.a potentially significant component of the transgressive systems tract: case study from offshore northwest Java. Laurin. Across platform 100’s of small circular buildups. R. Wu. Tide-influenced elongate large patch reefs in Kujung 2 and K 1 and Wonocolo Bibliography of Indonesia Geology. Kujung 1. V.0 186 www. Bima Field large field in Miocene Baturaja Fm carbonate buildup on flank of N-S trending basement high and underlying Talang Akar Fm sandstones) Ponto. Java Sea. Features asymmetric.Reservoir petrophysics of Bima Field. (AAPG) Bull. Wu.2-2. E..3 . (2001). Large build-ups off platform. 397-422. Ridges oriented parallel with axes of broad paleoembayments associated with structural fabric of basin. Mtg. Wonocolo buildups larger than Kujung buildups and have clinoform architecture: circular to elliptical.0 km wide. Jakarta. Geol. and have significant exploration potential.R.W. 4-10 km wide and up to 20 km long.W.H. Soc. (IPA). >20 km long. George et al.Improved interpretation of the Talang Akar depositional environment as an aid to hydrocarbon exploration in the ARII Offshore Northwest Java contract area: Proc. Smaller patch reefs 60-120 m diameter at tops of buildups. New interpretation determined four environments: continental.C. 17th Ann. Shelf ridge deposits tend to be sand prone and overlie ravinement surfaces. Morgan. 6th Regional Conf. Indon. Small Kujung 2 patch-reef buildups <120.A. (Images of Miocene carbonate landscapes from 3D seismic off N Madura.. A. p.W. Post Wonocolo basin subaerially exposed and veneered by fluvial systems. 86. (extended abstract) (Buildups N of Madura range from small patch reefs to platforms with outliers. Pranoto & W. Jakarta 1987 (GEOSEA). C. 10. Purantoro (1988). with ~25-40 m of relief. and tide influenced elongate large patch reefs in Kujung 2. 6. 85. H. and up to 17 m high.) Cenozoic carbonate systems of Australasia.. N. Conv. Buildups within platform 600m. Spec. (2002). H. Geoph. (Mapping of porosity on petrophysically calibrated seismic data. American Assoc.D. 1771-1793. Sedimentary Geology (SEPM). 75-106. A. Geol. & P.V. Petroleum Assoc. Clastic low-angle clinoforms from NNW beween deposition of Kujung 1 and Wonocolo Fms. (Oligocene Talang Akar Fm previous facies interpretation deltaic and marine. In: B.. 17th Ann. Drajat (2010).5 km wide tidal channels) Posamentier. (Miocene unincised and Pleistocene incised valleys imaged on 3D seismic on shelf offshore NW Java) Posamentier. (eds. Situmorang (ed.H. C. Pranoto & W. Anastamosing 200m deep. Jakarta. and Wonocolo Fms. Houston 2005. Geology Mineral Hydrocarbon Resources of Southeast Asia.Controls on hydrocarbon accumulation in the Main. Four cycles of delta progradation from northern source) Posamentier. (IPA). p. p. Soc. Roe & R. p. Stinson (1988). Delta complex and shore zone good source and reservoir potential.6.361. Publ.5 km. In: W.H. Proc. delta complex.vangorselslist. (3-D seismic of Miocene off NW Java shows extensive shelf ridge deposits: linear bodies 0. Massive sandstones of the Upper Cibulakan Formation.2.Seismic geomorphology of Oligocene to Miocene carbonate buildups offshore Madura. 4p. These deposits migrated across ancient sea floor. A. Petrol. P. represent important component of transgressive systems tract. Laurin (2005). Ridges formed as result of erosion and reworking of sand-prone deltaic and/or coastal-plain deposits by shelf tidal currents. H. H. Indon. 345. 95.W. Four stages in Talang Akar Fm depositional history) Ponto.. 1. p.2 km diameter and 200-300 m thick. Indonesia.Seismic stratigraphy and geomorphology of Oligocene to Miocene carbonate buildups offshore Madura. shore zone and shelf.500 m wide.Ancient shelf ridges. (SEG) 2005 Ann. immediately after shoreline transgression.) Proc. Buildups range from small patch reefs to platforms with outliers.Poggiagliolmi. 1.H. 175-194. Assoc. Sumantri.tectonic episodes: (1) Some of Pre-Tertiary and economic basement show compressive regime (subduction/ collision). (2) Most of DBS Paleogene extensional regime.5 km wide. p. 1. In: Int. Indonesia 9. normal to platform. H. implications for hydrocarbon prospect. Suyenaga. JCB2015-110. F.Structural and tectonic development of West-East Indonesian backarc transition zone. Basement consists of mixed oceanic. Sarmili (1994). 23-60. W. Situmorang & S. Inst.V. HAGI-IAGI-IAFMI-IATMI. Sugeng H. offshore northwest Java. Back arc region of E Sunda arc currently closing) Prasetyo. Biostratigraphic and sedimentologic data indicate open marine channel-fill. Conv. 26th Ann. T. (1992). p. R. Balikpapan. gravity. while Bali Basin represents analog of initial stage of foreland fold-thrust belt. Proc. Dwiyanto (1986). Indonesia. & L. 6. (IPA). Proc. suggesting multiphase deformation. M Miocene and younger basement-involved inversion to form 'Sunda Folds'. & B.2–2. Bull. Geol. Djatmiko (1997). Indonesia 2. likely deltaic. At least five geologic. Larger circular to elliptical patch reefs of Kujung 1 coalesced to form NW-SE trending platform. H. Flexure of SE Sunda shield margin to S beneath volcanic ridge.. a NE-SW and E-W series of ridges and deep basins in E Sunda Backarc. p. Conv. 20 km long). Bull. Back arc portion of the DBS currently closing and will form suture zone in future) Prasetyo. 58-70. Pratama. H.First screening method use in low contrast low resistivity pay evaluation of the upper Cibulakan reservoirs in the L Field offshore Northeast Java.2 km wide and 200-300m thick. 2.Fms.The 'Doang Borderland System' in the Southeast Sunda Shield margin: implications for hydrocarbon prospect in the eastern Indonesia frontier region. Indonesia. Ed. side-scan seafloor mapping and Airborne Laser Flourescensor data used to determine geologic-tectonic development of “Doang Borderland System”. Hundreds of small circular buildups of Kujung 2 range from 120 m. and (5) Backarc fold-thrusting since Neogene. related to collision of Buton micro-continent with Sulawesi arc. Seminar on the sea and its environments.. Petroleum Assoc. T.Sunda Arc collision and Roo Rise (oceanic plateau) subduction in Sunda Trench. Conv. Large buildups form off platform. p.Stratigraphic analysis of the Main Member of the upper Cibulakan Formation at E field. Rufaida. Tectonic phases: 1. H.com Sept 2016 . Ikhrandi.0 187 www. Prasetyo. Proc. drill-holes. Buildups within platform 600m. Jakarta. Marine Geol. Petroleum Assoc. Smaller patch reefs at tops of buildups. 4. Utomo & R. continental and Paleogene volcanic rocks. Joint Conv. Y. showing oceanic crust of Flores basin currently closing) Prasetyo. 3-11. 1-6. Pemberton (1998). & W. 21st Ann. and 25-40 m of relief. Main Member imaging reveals sand fields or patches. (4) Flexural downbowing to S of SE Sunda Shield margin (N basin margin) alongN Sunda volcanic ridge.W. 3.The Bali-Flores Basin: geological transition from extensional to subsequent compressional deformation. D.Single channel seismic reflection study of the eastern Sunda backarc basin. p. (W-E Indonesian Backarc Transition Zone (WEIBTZ) in E Sunda Arc System between Makassar Strait to N Bali and to E by NW-SE trending submarine ridge N of Flores. associated with Australian margin. 455-478. Paleocene rifting. Nugroho. in which oceanic crust of Flores Sea subducted S-ward beneath arc. Fathurrahman. Anastamosing channels up to 200m deep and 650m wide.R. 2. 129-153. (Amplitudes in Upper Cibulakan Fm at E Field show E-W trending channel. up to 400 m thick. H. North central Flores.5 km wide) Posamentier. Back arc thrusting N of Lombok reflects initial stage of arc polarity reversal. Indon. Clastics low-angle clinoforms from NNW.. 26th Ann. 1. Proc. p. 10p. Top Wonocolo Fm subaerially exposed and site of densely spaced fluvial systems. (IAGI).Bawean island as a new geoturism destination in East Java basin. A. Woncolo buildups larger than Kujung (4-10 km wide. Ujung Pandang 1995. Wirasantosa (1995).500m in diameter. H. (Seismic.G. Indon. Marine Geol.. Inst. Neogene back arc foldthrust zone. with internal clinoforms and separated from each other by tidal channels 1. Indon. interpreted as sand waves migrating across a transgressive surface of erosion) Prasetyo. Bibliography of Indonesia Geology.. (Young back-arc thrusting N of Bali-Lombok-Flores. Amami (2015). Westward transition from well-defined accretionary wedge to fold structural styles indicates W-ward decrease in shortening. Meyrick & S.W. (3) extensional regime inverted to form 'Sunda Fold' structures. associated with Australian margin-Banda Arc collision and subduction of Roo Rise oceanic plateau in Sunda Trench S of Bali.vangorselslist. B. a sleeping giant. First drilled in 1974 by ZZZ-1 well. Five coral-algal-foraminiferal limestone facies distinguished. Upper Cibulakan Group.Lombok basin. Coarser grainstone.0 188 www. Balikpapan. but at that time deemed non-commercial and heavy oil) Priyono. & W. Jauhari & W. (Reservoir sand distribution in fluvial 35-1 sand in Gita Mb of Talang Akar Fm in Widuri Field) Ralanarko. Gas analysis: methane (98. J. Yogyakarta. (M Miocene Mid Main Carbonate sequence in Seribu Shelf area of NW Java Basin comprises numerous N-S trending reef build-ups. 6p. Kaldi & C. offshore Ses Block. D. S. With outcrops of Late Oligocene. 4th Circum Pacific Council for Energy and Mineral Resources Conf.Pliocene quartz sandstones and Pleistocene volcanics. 37th Ann.) Trans. Joint Conv. Wijaya. offshore Southeast Sumatra. based on gas isotope lightness and low C2-C7 content. Butterworth. P. D.Shallow gas in ASRI Basin. Lantung. HAGI-IAGI-IAFMI-IATMI. indicated by decrease in C29 sterane relative abundance from 70 to 30%) Ralanarko. 41st Ann. 5p. (1987). Horn (ed. M. 1. Conv. Proc. J.Reservoir characteristics and petroleum potential of the mid main carbonate. ('Asri Basin in W Java Sea with cumulative oil production of 549 MMBO. Gas 99% methane and viewed as biogenic. p. Radke..19%). Conv. 23rd Ann. Indon. Jakarta. Northwest Java Basin. G-068. Late Miocene.. Sun Pengxiao & Su Chonghua (2015). Assoc.G. Indonesia. Geochimica Cosmochim.L. Acta 58. 2/3 of oil in partly stratigraphic trap of E Miocene Baturaja Limestone. Stable isotope data show gas unlikely to be biogenic gas without thermal hydrocarbons) Ratkolo.Bima Field. (HAGI). p. The latter processes with greatest effect on porosity and permeability. H..com Sept 2016 . (IPA). 289-306. Asri Basin. A. (IPA). Geophys. J. p. 2012-E-11. (C1-C3 naphthalenes and cadalene determined in 60 crude oil samples from Sunda. Singapore 1986.vangorselslist. Oils from Ardjuna and Jatibarang basins mainly derived from terrestrial sources. Vriend (1994).Petroleum potential of the East Java. Petroleum Assoc. Indon.Geochemistry analysis for reoptimizing a gas well to be developed case study: ASRI Basin. Senoaji (2012). Widjonarko. wetness 0. R. Indonesia. (IAGI).9%). Indonesia: drilling hazard or future potential? Proc. Ed. Larger pores mainly secondary vugular or fracture porosity (23%. Senoaji (2012). 6.K.. Secondary target now is gas in Air Benakat Fm. Proc. Proc. Indonesia.D. Indon. (General paper promoting hydrocarbon potential) Purantoro. Jakarta. 3675-3689.W.. Assoc. Rullkotter & S. P. Conv. p. Transition to marine depositional environment in Sunda basin. Oil seep at in Mt. offshore NW Java. PITHAGI2012-065. S Bawean) Prior. Conv. Adhiperdana (2007). (1994). E.E Miocene limestone.(Geotourism potential of Bawean Island on Bawean Arch.50 %. Southeast Sumatra. Gunawan. Palembang. Main diagenetic processes early diagenetic marine and vadose cementation. R. 199-212.packstone facies locally reduced porosity by cementation Bibliography of Indonesia Geology.Uncertainty on stratigraphic heterogeneities within West Area and East Area of Widuri Field. In: M.Distribution of naphthalenes in crude oils from the Java Sea: source and maturation effects. (Shallow gas in Air Benakat Fm sandstone reservoirs in Susana-01 around 1600. Geol. R.. Indonesia: identifying 351 interval thin reservoir as an upside potential from fluvial channel system in Talangakar Formation. 6p. Indon. Gas accumulations can be identified as bright spots on 3D seismic. Sunardi & B.J. Ph. Additional pay in deeper Talang Akar Fm sst. Petroleum Assoc. Nugroho. Thesis University of Wollongong. 12p. with ~100 MBO of recoverable reserves. Proc. JCB2015-368.1800' TVD and and in other wells at ~1400'. Most probably generated from shale in M-L Miocene Air Benakat Fm) Ralanarko. Atkinson (1994). followed by later dissolution and cementation. P. (On large ARCO Bima oil field. offshore Northwest Java Basin: insights from U-11 Well.A sequence stratigraphic model of the Upper Cibulakan sandstones (Main Interval). T. E Java Sea.D. Sangkapura district. North and South Makassar Strait and offshore Kutei basin. Talang Akar Fm main productive reservoir. D. Arjuna and Jatibarang basins and in sample of Oligocene Talang Akar Fm resinite. 31st Ann. with tops in 30-50m water depth. G. P.E Miocene and was major source of clastic material to nearby depocenters. indicating tropical land-plant precursor) Ramsay. United Nations ESCAP CCOP Techn.A. Several exploration wells with high CO2 in Tuban Fm sandstones and Bibliography of Indonesia Geology. Vol. Coral Reefs 6. which includes Madura Island. JAV11-JAV13. 11p.V.(e. (IAGI). Reynolds. & L.V.Exploration and development of a new petroleum province. Phipps & L. p. Caughey et al. Publ. Phipps & L. Bandung. 161-172.Morphology and sedimentology of Halimeda bioherms from the eastern Java Sea (Indonesia). 6. Fewer and thicker along deeper S margin. In: Proc.0 189 www. Good quality reservoirs >10% recovery efficiency.D. (2014). nutrient rich S-moving Pacific Throughflow water from Makassar Strait) Roberts. like JS-I-1 ridge. No reef-building corals below 15m. S.H. 371-374. Main source of gas inMuriah basin.H. Geo-Marine Letters 7. Conv.termogenik pada area tinggian Bawean. Smaller offshore highs. nutritive water responsible for high Halimeda productivity and large bioherm development) Roe. stable northern platform (Java Sea) and series of deep basins to S (onshore). ARII ONWJ contract area: the search for additional reserves.. In: C. E Java Sea. Indon. Geol. C.com Sept 2016 . Java Sea. C.846. eastern Java Sea (Indonesia): a side-scan sonar study. NE-SW trending Bawean Arch dominant positive feature offshore. Proc. Proc.W.) Seismic Atlas of Indonesian Oil and Gas Fields. 43rd Ann. oleanane and high pristane/phytane ratio. Petrol. Effendi (1987). Nedom (1973). J. E Java Sea. Thickness up to 52m above Top Pleistocene surface. J. Ed.V. 22 nd Ann. Jakarta.Studi pendahuluan potensi gas biogenik. p. Natuna and Irian Jaya. Gas in Kujung Fm in Lengo-1 well mixture of hydrocarbon (67%) and non-hydrocarbon gas (CO2 13%.thermogenic. 1. (1993).Northeast Java Basin. Kalimantan. p. Muriah basin. Roniwibowo. A. E-W trending Rembang inversion zone. trend parallel to arch and separated by grabens and half-grabens with Eocene-Oligocene source rocks.Reservoir distribution of the Upper Cibulakan Formation in the Seribu Shelf MMM area. Indonesia. 50 m) and developed over large areas by coalescence of individual mounds. Morphologies range from small mounds (10–20 m diameter) through haystack features (100 m diameter) to broad swells. Oil from Mid Main Carbonate reservoir characterized by presence of bicadinane resins. Indonesia.g.. Seminar Generation and maturation of hydrocarbons in sedimentary basins. 7-14. 14% porosity and low permeability in Coral Limestone facies). 3-4..Morphology of large Halimeda bioherms. cekungan Muriah. Manila 1977.Semanggi. 832. Assoc. Carbon isotopes indicate gas is biogenic.Kawengan fields) Roberts.J.vangorselslist. H. Technology 25. separated by 30-40 km wide. Geology 15. Phipps (1988). 180-194.L. (1995). With stratigraphic column and regional seismic line Trembul. 4. (The most extensive.J.Ledok. Nitrogen 20%). (Bioherms composed mainly of Halimeda plates on Kalukalukuang Bank. ('Preliminary study on the potential for biogenic-thermogenic gas in the Bawean High area. (Halimeda bioherms along W and S margins of Kalukalukuang Bank. Indon. Laut Jawa Timur Utara.H. & H. Conv. 2. Assoc. H. which remained emergent from Eocene . p. Features average 20-30 m thick (max. Presence and growth rate possibly related to upwelling of deep.R. (Early paper on first 10 oil-gas discoveries made in offshore NW Java basins since exploratory drilling started in 1968) Reksalegora. or mixed biogenic. 6.Source rocks for oils in the Ardjuna sub-basin of the Northwest Java basin. and thickest Halimeda bioherms reported from modern seas are along margins of Kalukalukuang Bank. Numerous bioherms at N bank. p. 2: Java. (NE Java basin rel. 395-401. p. 50-70 km E of central Sunda Shelf. Upwelling of cold. North East Java Sea'. Effendi (1987). Aharon & C. Polito (1977). H. PIT IAGI 2014-115. Geol.Halimeda bioherms of the eastern Java Sea. (eds. Indonesia. Upwelling of cold water and nutrient overloading from Pacific Troughflow water possible explanations for remarkable algal growth at expense of reef-building corals) Roberts. H. (IAGI). p. Proc. Locally high CO2 content in gases in region. (IPA). probably magmatic activity. 4p.Organic geochemistry as an aid to exploration in the East Java Sea. Arifin (1994).. 6. (3D seismic interpretation of Oligocene-Miocene carbonate buildups of N Madura Platform. A. Hughes (2008). in other wells derived from organic activity) Roniwibowo. Co-ord. J.0 190 www. Sturrock & A. 4.A.72m thick. One thick peat layer S of Masalembo 0. Kuntoro. Inst. (2015). East Java basin. 10p.Biogenic gas exploration in the Bawean High offshore North East Java Basin. Conv. domal buildups. (Similar to above.Preliminary results on the occurrence of peat deposits in eastern Java Sea. 2.M. Search and Discovery Art. (Ujung Pangkah oil-gas field offshore E Java with complex Early Miocene Kujung I (Prupuh FM) carbonate reservoir: E-W trending platform margin reef build-up with steep southern margin. (IPA). Saint-Cyr 2012. Indon. in coal beds and shale) Ruf. Bawean High and E Florence Basin.. Jakarta. Sutton & W. mainly of inorganic (magmatic) origin) Ruf...Petrophysical assessment for early water production in the Ujung Pangkah Field. Petroleum Assoc.Quantitative characterization of Oligocene-Miocene carbonate mound morphology from 3D seismic data: applications to geologic modeling. 34th Ann. CO2 in Lengo-1 gas derived from inorganic source.M. 87-96.vangorselslist. Simo & T. 30th Sess. p. IPA15-G-285.Insights on Oligocene-Miocene carbonate mound morphology and evolution from 3D seismic data. This confirms Kalimantan and Java were connected during Quaternary. (Extended-Abstract) (online at: www. Petroleum Assoc. Proc. Faturachman. Bangkok.5% and sufficiently mature) Shofiyuddin & S.S. kaolinitic and marine deposits.A. 69-80. 5th Ann. Reservoir Miocene Kujung Fm fractured carbonate with good to excellent matrix reservoir quality) Bibliography of Indonesia Geology. (IPA). p. A. Ilahude & D.com Sept 2016 . Indonesia. Bull. Fundamental controls on flow in carbonates. (IPTC). Petroleum Assoc. drilling losses. and outcrop data. 9-20. In: Proc.S. 120090. Meyers (1976). Indon. Hidayat (2013). Conv. which coalesce into amalgamated platforms (>5 km diameter)) Russell. S. (Non-marine and marine sediments on E Java Sea seafloor between Madura and Kalimantan include channel. volcanogenic. production. Proc. C.searchanddiscovery. with the Sunda river flowing in middle of area) Smart. Hughes (2008). Indon. closely spaced. 32nd Ann. Jakarta. J. Petroleum Assoc. M.C. p. Indon. D. 1-11. Kuala Lumpur 2008. (English version of Roniwibowo (2014). D.Kujung Fm limestones.com/documents/2013/120090smart/ndx_smart. (3D seismic interpretation of N Madura Platform shows growth history of Oligocene-Miocene carbonate buildups. Int. Conf. IPTC 12511. Proc. the only unit with TOC >1. Farurachman. IPA10-G-030.pdf) (Ujung Pangkah Field is 1998 gas condensate field with oil rim just offshore NE Java. 2. Indonesia. East Java Basin. Proc. D. 39th Ann. Siregar (1994). Comm. Kuntoro. 9p. Widespread swamp deposits with peat layers in E Java Sea. Jakarta. Conv. M.A. with peat layers up to 0. with Sunda River flowing in middle of area) Situmorang. A. (East Java Sea Poleng field oils probably sourced from Kujung Unit III (Early Oligocene) shales. Sutiyono (2010). logs. Peat layers on Java Sea floor suggest land areas between E Kalimantan and E Java-Madura during the Quaternary. (IPA). Active biogenic source in Muriah Trough. Joint Prospecting Mineral Resources in Asian Offshore Areas (CCOP). AAPG Hedberg Conf. Ilahude & D. Jakarta. Ed. A. Simo & T.Distribution and characteristics of Quaternary peat deposits in eastern Jawa Sea. Petroleum Techn.Discrete fracture network modeling based on seismic data.. IPA08-G-093. swamp. Marine Geol.Ujung Pangkah Field. 14p. Conv. Mound initiation with small (<100-500 m). East Java. A.. Early water production suspected caused by mobile water through fractures and vuggy porosity) Situmorang.L. p. Same paper as below. Indonesia 8. K. which become nuclei for intermediate mounds (2-3 km).4m below sea floor in 30m water radiometrically dated as Early Holocene.. Indonesia. Proc. (IPA). Jakarta.W. Conv. p. Lawrence & S. Toralde & H. 31. Bowman & W. Jakarta.Development strategy in the BZZ Field and the importance of detailed depositional model studies in the reservoir characterization of Talang Akar channel sandstones. underdeveloped due to inability of seismic to image sandstones) Sukamto. Ronnie P. Proc. Offshore Northwest Java. (Offshore NW Java basin mature area. 105-118. S. Penetration of organic-rich. J. Ed.Underbalanced drilling challenges and benefits in a marginal high-pour-point oil reservoir in Sepanjang Island. Bibliography of Indonesia Geology. Mitchell (1998). Int. 1-17. (Asri Basin off SE Sumatra PSC recoverable oil reserves of ~500MMBO from nine fields includinge major Widuri and Intan oil fields.pdf) (Biomarker cluster analysis of 45 oil samples in Sunda-Asri basins shows 6 geographically separated groups) Subidyo. 1.B. L. Asri Basin.The state of the art finding new oil and gas reserves in an old and mature area. wax content 24. Proc.An example of 3-D AVO for lithology discrimination in Widuri Field. p.Organic geochemistry: 1. Jakarta. SPE/ IADC Managed pressure drilling and underbalanced operations Conf.A.applications in the deep Ardjuna Basin. Widuri Field offshore Southeast Sumatra. (IPA). S. Indon.E. Oil and gas in channel-type sandstones of Talang Akar Fm. Zaki (2010). Good geochemical match between produced oils and E Oligocene Banuwati Fm lacustrine shales) Sukaryadi. 283-288.W. correlate with bright seismic amplitudes on 3-D seismic data. Underbalanced drilling for new wells to improve reservoir productivity Sosrowidjojo. p. (2011). Indonesia. J. Geographic location of crude oils based on biomarker compositions of the Sunda-Asri basins. off SE Sumatra. Sukanto. Herbudiyanto & T.. F.academicjournals. In: Proc. Tijdschrift Kon. Kuala Lumpur 2010. Conv.Petroleum systems of the Asri Basin. The Leading Edge 15. & Benarto V. Proc 20th Ann. B.P. (IPA). p. Java Sea.The morphological history of the Java Sea.Smit-Sibinga.S. Oil from (Eocene) Ngimbang Carbonate reservoir mostly of heavy black oil with high pour point of 120°F.. Conv. part of Kangean PSC.S. Surabaya. mature source rock by Hariet-2 well in 1995 helped define primary petroleum system. Indonesia.0 191 www. I.L.9%. (Sepanjang field is marginal oil field on Sepanjang Island. 26th Ann. Himawan. Aldrich. Cinta Field... Siboro. Parigi carbonates neglected as targets because only gas. Smith (1996). Harmony.. J. 2. Smith. Indonesia. G. Petroleum Assoc. Atmawan T. G. Petroleum Assoc. 24th Ann.B. 1. Gilmore. T. Amplitude maps at Base Upper Gita horizon interpreted as NE-SW trending belt of meandering distributary or fluvial channels) Sosa J. Conv. Sinclair (1995). (IPA).D.. Conv. T. Indonesia. 185-200. (online at: www. Proc. although one accumulation has >200’ of column and holds >1 TCF gas. C. (2002). Rinehart & J. Geol. Example of U1 well. (1947). H. p. 12p. Sudarmono. specific gravity 0. (1991). Indon. Danahey. p. Nunuk. W.. R. p. Asri Basin. offshore Northwest Java Sea. Abdat (2003). Indon. Assoc. Armon. Palao. Suria. 4. Success rate in Parigi <30 %. 7291-7301. J. Proc. 28th Ann. p. p. 1. 193-223. Physical Sci. 419-451.L. Jakarta. (2001).com Sept 2016 .W. Commonly thick Parigi buildups only thin gas columns at top.org/article/article1380715460_Sosrowidjojo. Sunda Basin. 31st Ann. first discovered by ARCO in 1990. Petroleum Assoc. J. Jakarta. 291-312.8574 and API gravity 33. Petroleum Assoc. (IPA). 6.K.B.C. Nederlands Aardrijkskundig Gen.Characteristics and sandbody geometry of the 34-1 reservoir. Indon.L. Petroleum Assoc.Reservoir characterization study to delineate dimension of channel. Reservoir is tight Ngimbang Fm carbonate at depth of ~4600'. Indon.vangorselslist.Talang Akar (Oligocene) source rock identification from wireline logs. (IAGI). Indon. Conv. (Oil producing Lower Miocene U Gita Mbr sandstones of U Talang Akar Fm in Widuri Field. 29th Ann. E Java Sea. 6.. B. T. 572-576. F. 64. E. Sequence stratigraphy in SE Asia. Lemigas Scientific Contr. with organic matter from both marine and terrestrial sources. 327. Petroleum Assoc. 1. Satyana (2016). Petroleum Assoc. J.T. Indon. Jakarta. (eds. Crude oils from Paleogene Ngimbang Fm in Kangean oil field in offshore NE Java Basin classified as mixed oil.3. is another indication that there is Cretaceous source in area (proposed to be part of Australian-derived Paternoster-Kangean microcontinent.0 192 www. Sci. Butterworth. may correlate to Cretaceous age. Bachtiar (2015). 39th Ann. Techn. Musu (2015). marker for flowering plants) suggests oils originated from Cretaceous source rock) Sutanto. Presence of Lower Cretaceous Alisporites sp. deposited under oxidizing and reducing conditions. not necessarily Cretaceous.A. (IPA)..T. Soeprapto (2015). SE of Kangean. Proc. Musu (2014). Kawengan oil clearly terrestrial oil from deltaic source rock) Sutanto. Very low oleanane Index (<20%. (High Triaromatic Dinosteroid Index in 3 oil samples from Sepanjang Island 1. NE Java basin. Indon.W. Petrol.J. H. show stronger marine character and reducing conditions than typical Cenozoic 'Sundaland' oils and also show very low oleanane and sterane indexes.. Bachtiar & A.D. Occurrence of Alisporites sp. which may also be potential source rock. Jakarta. Atkinson. offshore Northwest Java. Indon.com Sept 2016 . Indonesia: evidence from biomarkers and new exploration opportunities.Application of oleanane and sterane index for biostratigraphic age determination: examples from Kangean oils. (NE Java Basin hydrocarbon source rock generally believed to be in Late Eocene.J. Subroto.Plio-Pleistocene seismic stratigraphy of the Java Sea between Bawean Island and East Java. p.T. H.Mesozoic source rocks in Northeast Java Basin. Proc. Petroleum Assoc. Musu. S. Indonesia: evidence from triaromatic dinosteroid. Int. & J. p. 23rd Ann. C. C. 145-159. 15-24. H. in sediments analyzed. 9p. (Similar to paper above: biomarkers in some oils from Eocene Ngimbang carbonates in Sepanjang Field.Application of integrated sequence stratigraphic techniques in non-marine/marginal marine sediments. Conv. H. indicating source of oils may be Cretaceous in age. M.A. Ed. (IPA). N of E Java and Madura. J.T. 17p.A. Sepanjang 1. (Abstract only) Susilohadi. Northeast Java Basin. Joint Conv.Marine depositional environment determination using hydrogen isotopic composition of individual alkanes: case studies from Kangean oils. 17p. 'Supports idea that Cretaceous source rocks were deposited in marine setting while Australia-derived microcontinent was drifting N-ward before it collided with SE margin of Sundaland in Cretaceous' (NB: If 'triaromatic dinosteroid' biomarker indicates Mesozoic and younger marine dinoflagellates and oleanane indicates (Upper) Cretaceous and younger angiosperm land plants. 3 oils may be from mixture of marine and terrestrial kerogens. Offshore Northwest Java. an example from the Upper Talang Akar Formation.) Proc. Gresko.D. Balikpapan. & J. couldn't the low oleanane/ high dinosteroid signify a marine Tertiary. Andani. Symp. (Marine geology/ seismic stratigraphy of SE part of submerged Sunda Shelf.vangorselslist.Mesozoic-aged oils in the Northeast Java Basin. source facies?. 5-16.4 wells. SE of Kangean in Java Sea.E Oligocene early synrift Ngimbang Fm. p. IPA15-G-090. (Geochemistry of oils from well in Kangean (Sepanjang) area. Petroleum Assoc. Multiple Quaternary erosional features resulting from exposure during major sea level lows) Sutanto.Suria. as also supported by previous studies reporting Oleanane Index <20%. Indon.H. Satyana & A. S.. but Cretaceous marine sediments are also known all around the Sundaland margin. Proc. 37. S.J. Proc. 6. Conv.. 1. A. which is common for samples from older sources than Cenozoic. Ardjuna Basin. Musu. Suria. Gresko & B. M. & T. Sinclair. JCB2015-207. Java Sea and Kawengan. Berita Sedimentologi 32. C. HvG)) Bibliography of Indonesia Geology. HAGI-IAGI-IAFMI-IATMI. 40th Ann. IPA16-663-G. Conv. low oleanane % suggests marine shale source. Jakarta. Caughey et al.W. A.H. N. P. HvG)) Sutanto. Atkinson (1995).. p. In: C. Sinclair & C. suggest presence of Cretaceous sediments. the Northeast Java basin. (IPA). Mahaperdana (1994). E. Jakarta.Sequence stratigraphic surfaces identified on conventional core data: Talang Akar Formation. Reservoir water saturation and permeability modeling in the Pangkah Field. Asian Earth Sci. 2012-GD-08. East Java. probably due to extension initiated in Late Eocene. Jakarta. Geol.Posisi tektonik Bawean-Muria dalam hubungan dengan hidrokarbon cekungan Cepu. (2009).Integrated petrophysics in Kujung carbonate reservoirs. Central Java'. Yogyakarta.. Conv. two shoal complexes with progradational and aggradational patterns at W to C part and E part of platform. 14th Ann. (1978). Assoc. (IAGI). E. A.. Manila 1977. Proc. p. (1998). During relative sea level lowstand topographic highs at center of shoal complexes might be exposed. Joint Conv. Surabaya 2005. 32 nd Ann. Indon. Geol. basalt andesite.. incl. p. & A. Proc. Koswara (1993).6 -0.Seismofacies study in early fill to source rock depositional environment. (2005). Dev. 34 th Ann. Jakarta. S. Indon. Asri basin. Sequence boundary is onlap surface. H. unconformably overlainby Late Miocene-Pliocene marine Brakas Fm limestone-sandstones) Sutiyono. S. JCS2005S029.Krisna Lower Batu Raja waterflood project. 11p.Sequence stratigraphy and depositional model of the Ngimbang carbonate reservoir in Pagerungan Utara offshore. offshore SE Sumatra. K. Java. 6. mainly N-dipping.Cenozoic thermotectonic history of the Sunda-Asri basin. (Eocene Ngimbang Carbonate isolated platform reservoir in Pagerungan Utara two depositional sequences. (Kangean and Sapudi islands folded Oligocene-Pliocene sediments. 5-6. (IPA). (On log interpretation challenges in E Miocene carbonate buildup of Ujung Pangkah Field. 1-8. Java Sea. Indon. Indonesia. 1808-4. O. IPA10-G-012. (NW Java basin oilfield development) Bibliography of Indonesia Geology. (IPA). Syafrie. Hariet-1 and Yani-2 in Sunda-Asri basin suggest basin continues subsiding. IPA09-G-022. 1.J. Geothermal gradients relatively constant through Cenozoic) Sutton. Bandung. Petroleum Assoc. Ed. & Reno F. J.Muriah in relation to the Cepu hydrocarbon basin. M. East Java. CCOP Techn.G. Java Sea) Sutriyono. scale 1:100. Publ. with significant amounts of leucite. Conv. Center. Upper part interfingers with Oligo-Miocene Tambayangan (= Kujung) orbitoid limestone. 163-179.0 193 www. 6. NE Ria-1. 169-194. Indon. A. and finally covered by hemipelagic shales (Ngimbang Shale)) Talo.com Sept 2016 . Composed of phonotepite.000. with ages of 0. C. (AFT analysis of Cenozoic rocks from wells Asri-1. Disiyona. Randall (1985). Proc. p. Jakarta.Geological map of the Kangean and Sapudi Quadrangle. Earliest fill alluvial-fluvial setting with N-S sediment transport direction. Bintoro W.P. (Seimic facies maps of Eo-Oligocene early basin fill of Asri Basin.0.26 M. Similar to Muria volcano (0. I. Subsequent relative sea level rise resulted in TST carbonate deposition (U Ngimbang Carbonate) only on platform with upward fining/deepening facies succession. Kangean Block. Tata & B. 41st Ann. Res. p. Banuwati lacustrine shale source rocks. 485-500. Recent heating of rocks consistent with 800m of Plio-Pleistocene burial. with local sediment sources from W and E flanks of rift basin) Takano. Petroleum Assoc. IPA08-G-062. Paper is on initial petrophysical models to calculate water saturation and permeability) Sutiyono. Bawean Island volcanics different from Java arc. offshore NE Java. Samodra & A. ('Tectonic position of Bawean.vangorselslist. 30th HAGI. (IPA). 16. p. Overlain by E-M Miocene Jukong-Jukong Fm limestone.Depositional environments and their relation to chemical composition of Java Sea crude oils. 34th IAGI. Proc. in front of present day Solo river delta. 1708-4. Proc. southeast Sumatra: new insights from apatite fission track thermochronology. 98-111. A. 1709-3. Indon. Usman (2012). Sudradjat & E. Petroleum Assoc.Sutisna.4 Ma)) Syarif. Heruyono (2008).67. Jawa Tengah. Petroleum Assoc. (2010). United Nations ESCAP. Main producing Kujung-I Fm is complex carbonate reservoir. Proc. Conv. Conv. In: Seminar Generation and maturation of hydrocarbons in sedimentary basins. 7p. Oldest rocks Late Oligocene Cangkaramaan Fm marls with planktonic forams. HST of lower sequence (L-M Ngimbang Carbonate). Jakarta. 33rd Ann. (Ujung Pangkah Field is 1998 discovery in E Miocene platform margin carbonate reef build-up. p. Conv. 14th PERHAPI. trachite and phonolite. A. (IPA). Temansji & R. W. 15th Ann. P. American Assoc. Jakarta. West Java Sea. p. Gravity data suggest thick Tertiary depocentre. Geol.Basement lithology and its control on sedimentation. After E Tertiary block faulting and nonmarine basin-fill. (IPA). A. 3..E Eocene. Himawan (1999). D. Jakarta. 29p. W.G. Local reversal of trend in Miocene along N part of CLB where shelf margin Bibliography of Indonesia Geology. Rel. Two stage rift model that progressed from E to W. P.) Changing face of East Asia during the Tertiary and Quaternary. (Central Lombok Block (CLB) N of Lombok/ Sumbawa underlain by Cretaceous melange and/or oceanic crust. SE Sumatra. Ed.Earliest Oligocene structures reasonable chance of capturing hydrocarbons) Tonkin. 123-140. 24th Ann. Tyrrell. p. Conv. Most of upper Paleogene and Neogene in deep water facies. By Late Eocene deep marine environment while areas to N had just been transgressed.32. Petroleum Geol.W.C.E.1-7. Conv.G. (Sunda Basin Cinta Field produces from Late Oligocene Talang Akar Fm sandstones and overlying Baturaja Fm reefal carbonates. Davies & H. Petroleum Assoc. Park (1992).) Carbonate rocks and reservoir rocks of Indonesia: a core workshop.Temansja. 1. 2.G.. 7. Cinta Field.E Eocene source rock reached peak oil by end Eocene. Indon.C. In: N.Reef complex lithofacies and reservoir. Siemers et al. (1997).Miocene carbonate shelf margin. Lidya field reservoir pinch-out onto eroded areas of basement silicification along shear zone. Widuri-Intan oilfields. Petroleum Assoc. p. Central Java. R. McDowell (1986). 47-75. Proc. Jakarta. Sunda basin. 2. Basement topography influenced subsequent distribution of fluvial channels and sand pinch-outs. In: C.) Atlas of seismic stratigraphy. Rama Field. P. W. Secondary porosity restricted to packstones of bioclastic debris from main reef. Southeast Sumatra. Basin modeling shows Paleocene. (3) plugs of metabasalt and related volcanic rocks.C. p. Reservoir sands interbedded with mudstone and coal and overlie Cretaceous basement rocks. In: A. so only Late Eocene. Conv. Indonesia. 6. Geochemical evidence of migrated hydrocarbons in dry wells. Oil in structural and stratigraphic traps in sinuous-meandering channel sandstones. Indonesia. Sandstones frequently large amounts of pore-filling kaolinite. p.New and significant fossil finds from Sangiran.Determination of permeability in sandstone reservoirs affected by diagenetic kaolinite. Proc.A model for hydrocarbon accumulation in Sunda Basin. Fourth Conf.An alternative view on the existence of an effective petroleum system in the Bali-Lombok area. (eds. except along E and N margins where shallow water carbonate banks were progressively drowned.C. Faults controlled by basement lithology.com Sept 2016 . P. (1995). Ppt presentation SEAPEX Conf. 174-179. (IPA). NW-SE shear zone offset basement between main Widuri and Intan fields. p. Petroleum Assoc. Indon. (Five main lithofacies in Rama field E Miocene Baturaja Fm. (2) metamorphic rocks (mainly mica schist). (2007). (IPA). 22. 1. minor in-situ reef facies tightly cemented poor reservoir) Tyler. (Widuri-Intan fields in NW Asri Basin produced ~310 MB Oil from Late Oligocene Talang Akar Fm fluvialdeltaic sandstones. 141-165. (4) dolomitic limestone. especially at boundaries of intrusives. & R. 45-59. (Bali-Lombok area water depth 200-1000 m and extension of E Java Basin. from breakdown of potassium feldspars from volcanic detritus) Tonkin. Evolution of the East Asian Environment. Marine transgression progressed from SE to NW.Miocene carbonate shelf margin. (IPA). & D. Bushnell (1986). Reservoir at Indri field underlain by dolomitic limestone and exhibits karst sinkhole and collapse structures) Tonkin.0 194 www. & R. By end M Eocene Bali-Lombok area fully marine. A. Jablonski (ed. trap formation and hydrocarbon migration. part of Paleocene and M Eocene rift system that developed between. Proc. Tognini. (AAPG). Indon. Proc. Petrol. Drape and compaction over eroded volcanic plugs enhanced structural-stratigraphic plays. Petroleum Assoc. Davis (1987). Jakarta. J. Studies in Geology 27. 15th Ann. Bali-Flores Sea. Indon. p. (Amoco seismic line showing SW prograding Miocene carbonate shelf margin) Tyrrel. Basement lithologies: (1) hornblende granodiorite.K.W.T..D. Singapore 2007. Bali-Flores Sea. 498-515. Potential lacustrine and paralic source rocks only in Paleocene. area underwent rapid subsidence. Bally (ed. Southeast Sumatra.vangorselslist. Caughey. (IPA). but accumulations not commercial due to unpredictable reservoir quality. (E Java Sea Sakala Timur area basin modeling by BP. Carter et al. Meratus trend and Muria. Most effective way to find carbonate reservoirs is to use seismic attributes in combination with the conventional methods of seismic interpretation such as structural mapping. M. 379-415. (Poleng Miocene carbonate reef off Madura once abandoned field revived as economic venture after 3-D seismic survey. Armon & S. MacGregor (1996). Petroleum Assoc. Petroleum Assoc.C.W. Several small discoveries in recent years. M. and led to new discovery at KE-23 Field) Welker-Haddock. Park. S. (IAGI). Java Sea.W. Petroleum Assoc. I. Semarang. (IPA). (Seismic response to variations in lithology is complex and non-unique. Topseal capacity of silty Tertiary mudstones main risk) Welker-Haddock.Tektonik dan jalur volkanik busur belakang Bawean Muria sebagai pengontrol pembentukan Cekungan Pati dan potensi hidrokarbon. Assoc. Present day top ‘oil window’ 9. (IPA). P.com Sept 2016 . 9p. R. J. Petroleum Assoc.A. In: C. Netherwood. 25th Ann. Drainage areas identified. isochron mapping to determine the paleogeography and seismic morphology) Wicaksono Prayitno. Azmalni. or low recovery factors. 111-118. Jakarta.. (online at: http://download. 421-435. Reason for failure of ST-Alpha well was lack of suitable migration pathway from mature source kitchen to trap. A. p.F. Conv. Indonesia. p. 1. A.P. Applied Sci. Nguyen (2001).R. F. from seven fields. R..Deep hydrocarbon play in Banyumas sub-basin. (IPA). Hanggoro (1996). Lodwick. W.The transformation of Poleng Field. Kahfi & Alfardi A. Indon. Sudarmono (1996). Indon. (Lower Miocene Batu Raja Fm and Gumai Fm shallow marine limestones 250 MMBO. Volcanics in area of Gunung Muria calc-alkaline-shoshonite magmas. p. Central Java: opportunities and risks.php?article=104220&val=1389) ('Tectonics and position of Bawean-Muria back-arc volcanic arc as controlling the Pati Basin and hydrocarbon potential'. 6. Petroleum Assoc.) Proc. A. (Sunda Basin good match between oils and Banuwati Fm lacustrine shales Type I kerogens. Indon. Jakarta. B. & D.D. p. D. p. Proc.K. Bibliography of Indonesia Geology. Indon.vangorselslist. Sequence Stratigraphy in SE Asia. Angkasa. 38th Ann.M.. PITIAGI2009-149. Geol. Conv. Conv. Jakarta 1995.S.2-D basin modeling of secondary petroleum migration in the Sakala Timur PSC. Proc. Proc. lateral migration dominates away from it beneath regional Gumai shale seal. Park & M. (IPA). Indonesia. limited areal extent.The implications of basin modelling for explorationSunda Basin case study. p.Use of sequence stratigraphy in carbonate exploration: Sunda Basin. 21st Ann. Indon. Mature source rocks more limted areal extent than indicated in earlier work.0 195 www.A. Asjhari.698. Jakarta. (eds. Budiarto & D. offshore southeast Sumatra. 25th Ann.portalgaruda. 28th Ann.500'. Indon. Bradfield & B. R.E. Wight.L. directional and horizontal wells. 2. Conv. 3.Bawean back arc volcanic belt divides NE Java basin in Pati Basin in W and NE Java Basin in E) Vear. Proc. 1. R. E.Prediction of carbonate sweet spots from 3-D seismic: a case history from Krisna Field.carbonate complex prograded ~9 km to SW over deep water basinal deposits during Miocene-?E Pliocene. Significant hydrocarbon generation began at end Talang Akar time in basin center and progressed outwards through time. Symp.R. 353-365.migration hydrocarbon system' delineate probable prospective areas) Wicaksono.org/article. SW-NE trending Muria -Bawean back-arc magmatic belt part of Quaternary volcanic belt on SE border of granite belt of Java Sea. Int. This was followed by rapid subsidence causing 'drowning' of N shelf margin after which slope was onlapped and covered by deep water Plio-Pleistocene mudstone) Usman. J. 197-229. Sequence stratigraphic study of carbonates undertaken to produce a predictive model for porosity development) Wicaksono. 681. Indonesian J. Vertical migration crucial close to generation area. Ed. 1. (2009). Jakarta. Haryono (1992). (2012). Proc. Boundaries of 'Banuwati generation. Conv. (On complex distribution of porosity and pore types in E Miocene Baturaja Fm carbonate reservoir in Kitty oil field. 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Pleistocene K-rich volcanoes behind active Sunda arc, at ~200-600 km above Benioff zone in E Java- Java Sea (Beser, Ringgit, Lurus, Muriah, Lasem, Bawean). Positions controlled by major faults oblique to Sunda arc axis. Origin ascribed to melting of mantle enriched in incompatible elements during previous events, e.g. Oligo-Miocene subduction beneath Java) Bibliography of Indonesia Geology, Ed. 6.0 217 www.vangorselslist.com Sept 2016 Soeria-Atmadja, R., M.E. Suparka & Y.S. Yuwono (1991)- Quaternary calc-alkaline volcanism in Java with special reference to Dieng and Papandayan- Galunggung complex. Proc. Int. Conf. Volcanology and Geothermal Techn., 10 p. Soetoyo, H.R.D. (1992)- Geologic map of Tangkubanparahu volcano (Sunda Complex volcano), West Java. Volcanological Survey Indonesia, 1:50,000 scale. Solikhin, A., J.C. Thouret, A. Gupta, A.J.L. 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Proc. 4th Pacific Science Congress (Batavia), Excursion E21, Vorkink, Bandung, p. 1-37. (Guidebook to Kelut volcano, E Java) Stehn, C.E., W.M. Docters van Leeuwen & K.W. Dammermann (1929)- Krakatau (Geologie, vulkanisme, flora en fauna). Proc. 4th Pacific Science Congress, Java 1929, Vorkink, Bandung, p. 1-118. (Fieldtrip guide book on Krakatau volcano, in 3 parts: (1) The geology and volcanism of the Krakatau group (Stehn), (2) Krakatau's new flora (Docters van Leeuwen) and (3) Krakatau's new fauna (Dammerman)) Stimac, J., G. Nordquist, A. Suminar & L. Sirad-Azwar (2008)- An overview of the Awibengkok geothermal system, Indonesia. Geothermics 37, 3, p.300-331. (Awibengkok (Gunung Salak) geothermal system liquid-dominated, fracture-controlled reservoir, hosted mainly by andesitic-to-rhyodacitic rocks, floored by Miocene marine sedimentary rocks cut by igneous intrusions. Major volcanic peaks of area built from 860-180 ka, while ancestral andesitic cone that forms rim of Cianten Caldera to W active from ~1610 to 670 ka) Sucipta, I.G.B.E. (2006)- Product of Lamongan volcano (Java, Indonesia): indication of gradational magmatic changes from continental to subduction-related system. Proc. Ann. Conf. Indon. Assoc. Geol (IAGI), p. Sudradjat, A. (1975)- Batuan gunungapi dan struktur geologi di Jawa Timur dan Nusatenggara Barat. Geol. Indonesia (IAGI) 2, 3, p. 19-22. ('Volcanic rocks and structure of East Java and West Nusatenggara') Sudradjat, A. (1981)- The morphological development of Krakatau Volcano, Sunda Strait, Indonesia. IAVCEI and Volcanological Survey of Indonesia, 18 p. Sudradjat, A. (1991)- A preliminary account of the 1990 eruption of the Kelut Volcano. Geol. Jahrbuch A 127, p. 447-462. (On 1990 violent eruption of Kelud composite volcano in E Java, after being quiet for 33 years. 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Major difference in eruption style between 20st and 19th centuries: in 20th century mainly growth of viscous lava domes and lava tongues, with occasional gravitational collapses of parts of oversteepened domes to produce nuees ardentes; in 1800s rel. large explosive eruptions with large “fountain-collapse” nuees ardentes) Vukadinovic, D. (1995)- High-field-strength elements in Javanese arc basalts and chemical layering in the mantle wedge. Mineral. Petrol. 55, 4, p. 293-308. (Quaternary basalts from Java-Bali sector of Sunda Arc show increase in high-field-strength elements (Nb, Zr, Hf) and decrease in Zr/Nb and Hf/Nb with increase of depth to Benioff zone, consistent with progressively enriched mantle wedge with depth) Vukadinovic, D. & I.A. Nicholls (1989)- The petrogenesis of island arc basalts from Gunung Slamet volcano, Indonesia: trace elements and 87Sr/ 86Sr constraints. Geochimica Cosmochim. Acta 53, 9, p. 2349-2363. Vukadinovic, D. & I. 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(Geothermal system of eastern Dieng volcanic complex, C Java, originated through intersection of two major fracture zones. Geothermal system is system of hot water and steam rather than dry steam only) Zen, M.T. & D. Hadikusumo (1964)- Recent changes in the Anak Krakatau Volcano. Bull. Volcanology 27, p. 259-268. Zen, M.T. & A. Sudradjat (1983)- History of the Krakatau volcanic complex in Strait Sunda and the mitigation of its future hazards. Bul. Jurusan Geologi ITB 10, p. Zirkel, F. (1875)- Leucitbasalt von Gunung Bantal Susum auf der Insel Bawean bei Java. Neues Jahrbuch Mineral. Geol. Palaeont. 1875, p, 175-176. ('Leucite basalt from the island Bawean near Java'. Brief letter on first discovery of first leucite-bearing basalts known outside Europe, from Gunung Bantal Susum on Bawean, Java Sea (leucite basalts also in Gunung Muriah, NE Java, and SW Sulawesi; HvG)) Zulkarnain, I. (2003)- Petrographic evidence for magma mixing beneath the Krakatau volcano and its implication for eruption magnitude and its mechanism. J. Riset Geologi Pertambangan (LIPI) 14, 1, p. 1-11. Bibliography of Indonesia Geology, Ed. 6.0 222 www.vangorselslist.com Sept 2016 III.4. Madura- Madura Straits Andrearto, W. & B. Syam (2010)- Carbonate reservoir prospect in Madura Island. Proc. 39th Conv. Indon. Assoc. Geol. (IAGI), Lombok, PIT-IAGI-2010-161, 5p. (Seven wells drilled in Madura island show carbonates in Madura Island have good reservoir potential. Prupuh Fm carbonates (N4, latest Oligocene- earliest Miocene) in S part of island bioclastic carbonates deposited in shallow marine- open marine facies with porosity 5-10%. Carbonate deposition in N relatively shallow marine and porosity 10-20%) Arifin, L. (2000)- Struktur patahan, lipatan dan akumulasi gas di perairan Sampang- Bluto dan sekitarnya, Madura, Jawa Timur. J. Geologi Sumberdaya Mineral 10, 103, p. 16- 22. (Shallow seismic reflection study at N Madura Straits. Several major anticlinal trends. Indications of biogenic gas accumulations) Arifin, L. (2001)- Akumulasi gas dalam sedimen de perairan Ambunten- Madura. J. Geologi Sumberdaya Mineral 11, 118, p. 19-25. ('Gas accumulation in sediments in waters off Ambunten, Madura. Indicators of shallow biogenic gas on shallow seismic lines offshore N Madura) Aziz, S., Sutrisno, Y. Noya & K. Brata (1992)- Geology of the Tanjungbumi and Pamekasan Quadrangle, Java (1609-2, 1608-5), 1:100,000. Geol. Res. Dev. Centre (GRDC), Bandung. (Geologic map of Central Madura. Folded Miocene- Pliocene sediments) Banerjee, B.R. (1993)- Seismic signature as a porosity indicator in Early Miocene reefs in the Madura Strait via AVO inversion and modelling. Proc. 22nd Ann. Conv. Indon. Petroleum Assoc. (IPA), Jakarta, 1, p. 445-481. (High porosity carbonate acoustic impedence can be similar to, or lower than, that of overlying sediments, whereas acoustic impedence in low porosity carbonate usually much higher than in overlying rocks) Boehm, A. (1882)- Ueber einige Tertiare Fossilien von der Insel Madura nordlich von Java. Denkschr. kon. kais. Akad. Wissenschaften Wien, Math. Naturw. Cl., 45, p. 359-372. ('On some Tertiary fossils from Madura island, North of Java') Edwin, A., K. Han & W. Nusantara (2013)- A case study on using Mundu-Paciran nannofossil zones (MPNZ) to subdivide Mundu and Paciran Sequences in the MDA Field, East Java Basin, Indonesia. Berita Sedimentologi 26, p. 26-32. (online at: www.iagi.or.id/fosi/files/2013/05/BS26-Java.pdf) (Reservoirs in MDA gas field in E Madura Strait are Late Pliocene planktonic foram grainstones and packstones, deposited as pelagic rains and redistributed by marine bottom currents across crest of Late Miocene inversion structure. Differentiating Mundu and Paciran Sequences (formation/ sequence names used onshore E Java) relies on biostratigraphy and chronostratigraphy, as lithologies are similar. Nannofossils used to define 8 local zones in NN11- NN18 (Late Miocene- Late Pliocene) interval. Best reservoir performance in latest Pliocene MPNZ-7 and MPNZ-6 zones) Endharto, Mac (2004)- The tidal flat-shelf depositional system of the Ngrayong Sandstone in the western part of the Madura Island. Proc. 33rd Ann. Conv. Indon. Assoc. Geol. (IAGI), p. 17-42. Endharto, Mac (2005)- The tidal flat-shelf depositional system of the Ngrayong Sandstone in the western part of the Madura Island. J. Sumber Daya Geologi 15, 2 (149), p. 61-80. (Gunung Geger-Gujug Laut-Water Fall section suggests M Miocene Ngrayong Sst in W Madura formed in tidal sand flat, from supratidal-salt marsh to shallow subtidal environments. Tabular cross bedding in bioclastic lithic arenite, interpreted as sand flat in headward portion of macrotidal estuaries. Overlain by marine transgression of Bulu Limestone with Cycloclypeus, etc.. Paleocurrents from cross bedding from N to S or SW direction (200°- 190°). Bibliography of Indonesia Geology, Ed. 6.0 223 www.vangorselslist.com Sept 2016 Tinjauan stratigrafi dalam tataan tektonik di Pulau Madura. Ed. Madura Straits. Northeast Java Basin. Int. (1992)..Guide Book Post Convention Field Trip. ('Seismic stratigraphy of Middle Miocene sediments in the Madura Straits area'.Early Miocene bioherm. p. HAGI-SEG Int.Peranan wrench fault pada akumulasi hidrokarbon di Pulau Madura. Despite carbonate lithology. All facies shallow marine. American Assoc. J. marl and bioclastic limestones with Cycloclypeus.pdf) (Outcrop study of lateral facies in Pliocene carbonates in Madura and Puteran Island.com Sept 2016 . R. Ass. Seismic stratigraphy study of Middle Miocene in S part of Madura Straits) Situmorang. Jawa Timur.8. KD. 1. 64. P. Conv. 6. NE Java) Pakpahan. probably windward side) Latief. Indonesian Petroleum Association (IPA). Geosc. Madura Island.Geology of the Waru-Sumenep Quadrangle. 213-232. ('Depositional environment of the Ngrayong member of the Tawun Formation in the Guluk Guluk area.. Hadiyanto & Y. (1986). East Java. p. (2007). Madura'. Agustianto& M. ('The role of wrench faults for hydrocarbon accumulation in Madura Island') Bibliography of Indonesia Geology. Exhib. Dev. Marl below sandstone with Globorotalia peripheroacuta. Jyalita & S. p. 12. (1961 hydrogeological inventory survey on Madura) Hageman. Sumenep. 21st Ann...Outlines of the hydrogeology of the Isle of Madura (Indonesia). (Unpublished) Mulhadiyono. p. Arakawa (2010). (AAPG) Bull. Geol. Surjono (2015).. Conf. 44-53. Harsono P. et al. Supriyadi. Sumenep. Orbulina) Purnomo. p. (Seismic study of four Miocene carbonate buildups in Madura Straits (Porong.A. No maps or other specific information)) Kusumastuti.Sedimentology and characteristics of Pliocene shallow marine carbonate as reservoir alternative based on outcrop analogue in Madura and Puteran Island. KE. 543-560. Centre (GRDC). Geol. D. 86.com/documents/2015/51212pakpahan/ndx_pakpahan. BD) on WSW-ENE trending Oligocene fault block.. Assoc.vangorselslist. Geol.S. P.P.S. & D. p. Berkeley. 487-488. 20-36. A.Nadere inlichtingen omtrent de op het eiland Madura ontdekte ontvlambare gasbronnen. Proc. scale 1: 100. p. Natuurkundig Tijdschrift Nederlandsch-Indie 24. M Miocene (zone N10-N13) Ngrayong Mb shallow marine sandstone. (IAGI). Brief communication on existence of gas seeps on Madura. Indonesia. N flank steeper.Flathe. IGCE10-OP-042.searchanddiscovery. Indon. Melbourne. (1862). Riset Geologi Pertambangan (LIPI) 7. Suparman (1983). ('Aditional information on the flammable gas seeps discovered on Madura'.K. indicating gas-water contact) Putra. H. buried by PlioPleistocene rocks.I. R. Hydrology. 2. B. Riset Geologi Pertambangan (LIPI) 17. (1990). 10 p. J. & Sukendar A. Res. Conf. 1. van Rensbergen & J.0 224 www. 1. N. Madura. Warren (2002). Jakarta. (Seismic imaging of Pliocene globigerinid packstones in Sirasun biogenic gas field. Geologi Indonesia.000. J.Lingkungan pengendapan anggota Ngrayong Formasi Tawun daerah Guluk Guluk. p. Porong buildup is Late Oligocene.Sekuen pengendapan sedimen Miosen Tengah kawasan Selat Madura. (New nomenclature for Tertiary of Madura. of Scient. Search and Discovery Article 51212.P wave-S wave sensitivity analysis of globigerinid carbonate in Sirasun gas field. 1. Pfeiffer (1963). J. Bali 2010. A. distinct flat spot present on seismic. 16p. Petrol.I. Bandung. A. (online at: www. unlike age-equivalent gas-bearing globigerinid limestone reservoirs in Madura Straits fields) Praptisih (1986). Proc. 207-222. AAPG/SEG Int.S.Seismic sequence analysis and reservoir potential of drowned Miocene carbonate platforms in the Madura Strait. In: Soc. p. Indon. p. (2015). 6p. Gas ~ 99% methane. 2. Engineers (SPE) Asia Pacific Oil & Gas Conference and Exhibition. low-resistivity case in clean-oil zones. Proc. Indon.H.php/IJOG/article/view/219/195) (Sequence stratigraphy and seismic facies of M-L Miocene interval in Madura Straits. Sharp (2007). Petroleum Assoc. Indonesia. Shanghai 1996. Suseno (1990). consisting almost entirely of Globigerina. Geoscience 2.id/index. Comm. & A. but in W. 25. case Study: Planning vs. Noeradi (2010). Harris. 2. (Extended Abstract) (In NE Java Basin Pliocene Mundu Fm Globigerinid sands carbonate with oil and gas MDA. Geol. Y. O and M fields. Wijaya. Y. as shown by widespread thin fluvial and alluvial fan deposits) Sutadiwiria. 77-87. land of opportunity.I.0 225 www.bgl.Susilohadi (1998). Basin with rapid subsidence and >200 m of Quaternary deposits. possibly on detached platform. primarily biogenic. Deposition interplay between Quaternary coarse-grained volcaniclastics deposition in S. Adelaide 2006. Gas column 49 m in Pliocene Paciran and Mundu carbonates. Coastal and Offshore Programmes E and SE Asia (CCOP). (online at: http://ijog. TSB. E Kendeng zone and Madura strait subaerially exposed. Conv. Jakarta. Marine Geol. and Quaternary sea level changes. A. discovered in 2006. Bull. Problems in reserves assessment include reservoirs compartmentalization (structural and stratigraphic) variations in depth of fluids contacts. 101-110. Ed. Prasetyo (2006). 31st Ann.3D properties modeling to support reservoir characteristics of W-ITB Field in Madura Strait area.C.) Triyana. Assoc.esdm. IPA07-G-115. During major sea level fall. Indonesian J. Maleo first offshore discovery of this reservoir type to be commercialized) Wahab. Structure partly filled 4-way closure. p.Quaternary sequence stratigraphy of Madura Strait. Tadiar & N. (Madura Strait characterized by syndepositional folding forming W-E trending basin between Madura and Java volcanoes. etc. Porosity up to 60%..go.The Maleo Field: an example of the Pliocene Globigerina bioclastic limestone play in the East Java Basin.vangorselslist. Coord. E. & H. Proportion of lime mud matrix primary control on reservoir quality. p. 362-383.250 m deep water. 6. Proc. p.Uncertainty in geophysic-geology-reservoir modelling for Globigerinid sand carbonate in NE-Java Basin. (W-ITB gas field in W part of Santos Sampang PSC. 2. SPE 100957-MS. (IPA). G. NW Madura Straits. marine fossiliferous mudstone from exposed Madura in N. Basden. Some oil production from Globigerina reservoirs onshore. Indonesia. Indonesia. 33rd Sess. Globigerina carbonates deposition in ~ 150. 2. W. G. 33-46. IAGI) 13.A. Geologi Indonesia (J. 45-61 (Maleo field 2002 discovery in Madura Straits. Petrol.Madura. In W-ITB 1 well gas reservoirs in Selorejo and Mundu Fms. which onlaps Top Early Miocene surface from N to S) Bibliography of Indonesia Geology. Indonesia. actual of fields development at Madura Strait. P.com Sept 2016 .Seismic and sequence analysis of Middle to Late Miocene deposits of Northeast Java Basin. & D.ITB 2 no gas reservoir in Mundu Fm) Yuniardi.