Biblio grap h yo f In do n es ian G eo lo gyBIBLIOGRAPHY OF THE GEOLOGY OF INDONESIA AND SURROUNDING ARE AS Edition 4.1, July 2012 J.T. VAN GORSEL I. REGIONAL GEOLOGY www.vangorselslist.com I. REGIONAL GEOLOGY The first chapter of the bibliography contains >180 pages with over 1900 titles of papers on the regional geology of Indonesia and adjacent SE Asia- Pacific, as well as general papers that do not fit in any of the regions or specialist categories listed separately. It is subdivided in five chapters: I.1. Indonesia Regional Geology I.2. SE Asia Tectonics, Paleobiogeography I.3. Volcanism, Volcanic rocks geochemistry I.4. Modern environments, Oceanography I.5. Carbonates, Coral Reefs I.1. Indonesia Regional Geology This chapter includes the references of textbooks and papers on the tectonics and regional geology of Indonesia. The Indonesian archipelago is an extremely complex collection of continental blocks, active and extinct volcanic arcs and associated subduction complexes (commonly with ophiolites, marking sutures where former oceans were consumed) and old and young ocean basins. It is now at the convergence of three major tectonic plates: Eurasia, Pacific and Australia. The area of Sulawesi contains elements of all three plates. A pre-plate tectonics depiction of 'tectonostratigraphic provinces' in Indonesia, fairly accurately grouping areas with similar tectonic histories, mainly based on similarities/ differences in Permian- Eocene stratigraphic successions (Umbgrove, 1938) Bibliography of Indonesian Geology v.4.1 www.vangorselslist.com July 2012 1 Western Indonesia ('Sundaland') is a complex of continental blocks that amalgamated in Late Paleozoic- Early Mesozoic time. Eastern Indonesia contains a number of small continental microplates derived from the Australia- New Guinea Gondwanan margin, now separated by young age oceanic marginal basins and volcanic arc systems. Many parts of Indonesia's tectonic history remain poorly understood. Numerous reconstructions have been proposed in the last 40 years since the acceptance of plate tectonics theory. Most agree on the broad relative motions of the three major plates, but they vary in many other details. Places like Timor, Seram, W Papua Birds Head, etc. continue to generate debate. Umbgrove (1938) lamented that 'in the last decades at least one or two new hypotheses have been suggested every year to explain the structure of the East Indian Archipelago'. Now, more than 70 years later, new models continue to be proposed and debated. Much progress has been made, but there is still no agreement on the 'final answer'. Suggested Reading Text books: Rutten (1927; remarkable understanding of Indonesian geology for its time; in Dutch), Van Bemmelen (1949), Umbgrove (1949), Hamilton (1979), Hutchison (1989), Darman and Sidi (1999). Tectonics, Reconstructions: Katili (1971, 1989, etc.), Pigram and Panggabean (1984), Rangin et al. (1990), Struckmeyer et al. (1993), Simanjuntak (1993-2000), Prasetyo (1995), Lee and Lawver (1995), Packham (1996), Simandjuntak and Barber (1996), Hall (1996, 1998, 2002, 2012 etc.), Hall, Clements and Smyth (2009), Harris (2006), Longley (1997), Villeneuve et al. (1998, 2001, 2010), Charlton (2000), Milsom (2000, 2001), Pubellier et al. (2003, 2005), Satyana (2003, 2009), Spakman & Hall (2010). I.2. SE Asia Tectonics, Paleobiogeography This chapter contains a large (>500 titles), mixed collection of papers on regional SE Asia tectonics, as well as papers on the tectonics and geology of parts of mainland SE Asia that are relevant to the understanding of parts of Indonesia (Thailand, S China, Myanmar, some Vietnam, etc.). Numerous papers on Paleozoic- Mesozoic faunas and floras are also included, especially those that help identify faunal and floral provinces indicative of paleoclimate and relative positions of plates through time. Paleobiogeographic patterns and stratigraphic successions are key tools underpinning plate reconstructions of SE Asia, especially in the pre-Cenozoic. The main patterns of the geologic evolution of SE Asia are reasonably well understood, but details and exact timing of events are still debated. SE Asia is a complex collage of continental blocks, all once part of the Gondwana supercontinent, separated from the New Guinea- Australia- India margin during multiple episodes of Devonian- Jurassic rifting (S China, Indochina, Sibumasu, W Burma, etc.). After Northward drift from the S Hemisphere to equatorial latitudes (recorded by changes in flora and fauna from colder to warmer climates), the various Gondwanan-origin blocks amalgamated with mainland Eurasia during multiple Late PaleozoicEocene episodes of collision. Multiple suture zones, many with ophiolites, represent the closing of a succession of ocean basins (PaleoTethys, Meso-Tethys, Neo-Tethys/ Indian Ocean) by subduction along the S Eurasia margin. These are accompanied by volcanic-plutonic arc systems and associated subduction complexes. Oceanic marginal basins formed by slab rollback after various collisions, some of which are already consumed, some of the Eocene and younger ones still remain (Andaman Sea, South China Sea, Sulu Sea, Celebes Sea, Banda Seas). Probably related with these are widespread Tertiary basins, mainly initiating in the Late Eocene-Oligocene. Several large strike slip fault zones, many still active today, further add to the complexity of the region. Suggested Reading Tectonics, Terrane reconstructions: Stauffer (1974-1986), Ridd (1980), Metcalfe (1988, 1996, 2009 a.o.) Sengor et al. (1988, 2009), Hutchison (1994), Hall (1997, 1998, 2002, 2009 a.o.), Pubellier et al. (2003, 2005), Satyana (2003, 2009) a.o. Bibliography of Indonesian Geology v.4.1 2 www.vangorselslist.com July 2012 1 3 www. Banda. Cretaceous. many additional papers that are specific to one area will be under the chapter for that area.vangorselslist.I. Volcanism.com July 2012 . Active volcanism occurs along four arc segments.recent magmatic arcs/ subduction zones Indonesian Archipelago (Katili 1974) Bibliography of Indonesian Geology v. unless they contain data or observations that are relevant to interpretation of the regional geology. With its 128 active and many additional extinct volcanoes. Indonesia has attracted volcanological studies for a long time. Most of the papers on modern volcanoes and descriptions of historic activity are not included. This chapter contains mainly papers on regional volcanism. the first three of which were probably once continuous and related to the same subducting Indian Ocean plate. Sunda. Volcanic rocks geochemistry Krakatau after 1883 eruption (Verbeek 1885). Sangihe and Halmahera.4.3. Soeria-Atmadja et al. ranging in age from Permian to Recent. Hartono (2009). deltas and deep marine environments and oceanography.). (2004). Modern environments. An understanding of this is obviously important to interpret the geological record. Siboga (Weber 1902). W Sulawesi) or the North ('Proto-South China Sea Plate': Kalimantan Cretaceous. Hoogewerff. 1989). Gupta (2005) Reports of expeditions Challenger (Brady 1884. Neumann van Padang (1936.1 4 www. Up to 15 older volcanic-plutonic arc systems have been recognized in Indonesia. 1930). Kuenen (1950). Bibliography of Indonesian Geology v. 1981). Hutchison and Jezek (1978).Philippine Sea Plate: Halmahera.1983). etc. post-collision New Guinea Late Miocene.M Miocene. Van Bergen. papers by Bellon. (1979) and many others I. starting in the last 3-6 Ma. Woodroffe (2005). Snellius (Kuenen 1935. Handley. Philippines. (1997) Kuhnt et al. the East (Pacific Ocean. Foden. (1986-2001) Volcanic rocks chemistry: Westerveld (1954). etc. Tomascik et al. 1974.vangorselslist. Carlile and Mitchell (1994). like tropical rainforests. Elburg.Banda Arc is quite young.4. Modern volcanoes and activity: Stehn (1927).Most of the volcanism in the modern Sunda. Vroon. Oceanography This section contains papers on modern environments and depositional processes in Indonesia.4.) and Snellius II (Van Hinte et al. Turner. Arc systems may be classified by age and whether the subducting oceanic plates were from the South (Tethys. etc. coral reefs. peat swamps. MacPherson. Eight of these have associated commercial mineral deposits. Whitford.Pleistocene) Suggested reading (see more complete listing in Van Gorsel 2009) Volcanic arcs through time: Katili (1973. A recent topic of great academic interest has been the flow of deep Pacific Ocean water to the Indian Ocean through the Indonesian Archipelago ('Indonesian Throughflow') and its imact on climate in the region. Suggested reading General text books: Oceanographic Expeditions: Physical Oceanography: Marine Geology: Indonesian Throughflow: SE Asia deltas: Ecology of Indonesia series. Harris (2006). Indonesia has been a study area for many types of modern environments. Gordon (2005 and others) Sidi et al.com July 2012 . Hutchison (1975. 1989) Wyrtki (1961) Molengraaff (1922. (2003). Indian ocean: most Indonesian arcs). Kusumadinata et al. I.5. Carbonates, Coral Reefs The Indonesia archipelago has long been a research area for the study of modern coral reefs. Early papers were by Molengraaff (1930), Kuenen (1933) and Umbgrove (1928-1947), more recent ones include Longman et al. (1993). Renewed interest in reefal limestone deposits came with the string of oil and gas discoveries in mainly Oligocene-Miocene age reefal buildup reservoirs on Java, Sumatra, Sulawesi and West Papua. A comprehensive overview of the widespread Tertiary limestones is Wilson (2002). Pre-Tertiary carbonates are relatively rare in Indonesia. Carboniferous- Permian limestones with fusulinid foraminifera are known from Sumatra, W Kalimantan- W Sarawak (Terbat Limestone) and Timor (papers by Fontaine, etc.). The E-M Permian of Sumatra includes the only true reefal Permian limestones in Indonesia (Guguk Bulat, W Sumatra). Late Triassic shallow water carbonates have been reported from Sumatra (Gafoer and Fontaine 1989), Bangka (De Neve and De Roever 1947), Timor (Vinassa de Regny 1915, Haig et al. 2007), E Sulawesi (Cornee et al. 1994, 1995, Martini et al. 1997), Buru (Gerth 1910, Wanner 1923), Seram (Wanner et al. 1952, Martini et al. 2004), Banda Sea (Sinta Ridge ;Villeneuve et al. 1994) and the Kubor terrane of Papua New Guinea (Skwarko et al. 1976, Kristan-Tollman 1986, 1989). Late Jurassic- Early Cretaceous shallow marine carbonates are present in Sumatra (Gafoer and Fontaine 1989) and W Kalimantan- W Sarawak (Bau Limestone). Deep water pelagic limestones of these ages are relatively widespread in Eastern Indonesia. Fractured Upper Triassic limestones are secondary oil reservoirs on Seram Island. Most of the references on individual carbonates are found in the chapters on areas in which they occur. Detail of Molengraaff (1922) map of modern distribution of coral reefs. Red = fringing reefs, Blue = barrier reefs and atolls formed as response to sea level changes, Green = barrier reefs/ atolls caused by 'diastrophism'. Uplifted coral reefs are common East of the yellow line. Bibliography of Indonesian Geology v.4.1 5 www.vangorselslist.com July 2012 I. REGIONAL GEOLOGY I.1. Indonesia Regional Geology Aadland, A.J. & R.S.K. Phoa (eds.) (1981)- Geothermal gradient map of Indonesia, 2nd ed.. Indon. Petrol. Assoc., Spec. Publ., p. 1-43 + 2 map sheets 1: 2,500,000. (Compilation of temperature data from petroleum wells in Indonesia. See also updated version by Thamrin & Mey, 1987) Abendanon, E.C. (1914)- Geologische schetskaart van Nederlandsch Oost-Indie, 1:2,500,000. Koninkl. Nederl. Aardrijksk. Genootschap, Smulders, The Hague, 6 sheets. (‘Geological overview map of the Netherlands East Indies’. First geological overview map of Indonesia, commissioned by the Netherlands Royal Geographical Society, The Hague) Abendanon, E.C. (1919)- Aequinoctia, an old Palaeozoic continent. J. Geol. 27, 7, p. 562-578. (Early tectonic interpretation of Indonesia. Presence of crystalline schists across E Indonesia suggests area from Borneo to New Guinea may all be parts of one ancient continent, stretching from Sulawesi to Tasmania, here named Aequinoctia) Adinegoro, A.R. Udin (1973)- Stratigraphic studies by the Indonesian Petroleum Institute (LEMIGAS). United Nations ECAFE, CCOP Techn. Bull. 7, p. 55-74. (Review of Cenozoic stratigraphic successions in NE Java, Jambi-Sumatra, NE Sumatra and E Kalimantan. One of first attempts to tie these local stratigraphies to global low latitude planktonic foram zonations) Ali, J.R. & R. Hall (1995)- Evolution of the boundary between the Philippine Sea plate and Australia: paleomagnetic evidence from eastern Indonesia. Tectonophysics 251, p. 251-275. (New paleomag from Sorong Fault Zone, Obi and Taliabu. Sula Platform Coniacian-Santonian paleolatitude at 19°+/- 6°, similar to Misool, suggesting Sula/Taliabu and Misool part of single microcontinent, >10° farther N than expected if attached to Australia, implying region separated from Australia before Late Cretaceous. Obi contains rocks of Philippine Sea and Australian origin. Volcanic arc at S edge Philippine Sea Plate collided with New Guinea at ~25 Ma, changing Philippine Sea-Australian plate boundary from subduction to strike-slip) Ali, J.R., S. Roberts & R. Hall (1995)- The closure of the Indo-Pacific ocean gateway: new plate tectonic perspective. In: F. Hehuwat et al. (eds.) Proc. Int. Workshop Neogene evolution of Pacific Ocean gateways, Bandar Lampung 1993, p. 10-20. Alzwar, M. (1986)- Geothermal energy potential related to active volcanism in Indonesia. Geothermics 15, p. 601-607. (90 geothermal areas identified in Indonesia, most located in active volcanic belts) Amiruddin (2009)- A review on Permian to Triassic active or convergent margin in Southeasternmost Gondwanaland: possibility of exploration target for tin and hydrocarbon deposits in the Eastern Indonesia. Jurnal Geol. Indonesia 4, 1, p. 31-41. (online at: www.bgl.esdm.go.id/dmdocuments/jurnal20090104.pdf) (Permian-Triassic magmatic-volcanic belts signify active Paleo-Pacific margin along New Guinea- E Australia part of SE Gondwanaland. Granitic plutons of S- type and may be tin-bearing. Back-arc basins of S Papua and Galille-Bowen-Gunnedah-Sydney basins filled by fluvial, fluvio-deltaic to marine Permian-Triassic sediments, locally with coal, unconformably overlain by marine Jurassic-Cretaceous) Anderson, R.N. (1980)- Update of heat flow in the East and Southeast Asian seas. In: D.E. Hayes (ed.) The tectonic and geologic evolution of Southeast Asian seas and islands, 1, Amer. Geoph. Union, Geoph. Mon. Ser. 23, p. 319-326. Angelich, M.T., R.L. Brovey, M.E. Ruder & C.C. Wielchowsky (1986)- Use of Seasat-derived free-air gravity to interpret the structure of Southeast Asia. Proc. 15th Ann. Conv. Indon. Petrol. Assoc. 1, p. 1-18. Bibliography of Indonesian Geology v.4.1 6 www.vangorselslist.com July 2012 (In areas of low sea-bottom relief SEASAT-derived gravity data can be treated qualitatively as low-pass-filtered Bouguer gravity field. Examples from SE Asia) Astjario, P. (1995)- A study of the uplifted coral reef terraces in the eastern part of Indonesia. In: J. Ringis (ed.) Proc. 31st Sess. Comm. Co ord. Joint Prospecting Min. Res. Asian Offshore Areas (CCOP), Kuala Lumpur 1994, 2, p. 116-121. Audley-Charles, M.G. (1965)- Permian palaeogeography of the northern Australia-Timor region. Palaeogeogr., Palaeoclim., Palaeoecol. 1, p. 297-305. (Autochthonous Permian rocks of Timor were derived as detritus from Kimberley region of N Australia. This conflicts with suggestions of large crustal dislocations immediately N of Australia recently advocated on basis of regional palaeomagnetic studies) Audley-Charles, M.G. (1966)- Mesozoic palaeogeography of Australasia. Palaeogeogr., Palaeoclim., Palaeoecol. 2, p. 1-25. Audley-Charles, M.G. (1976)- Mesozoic evolution of the margins of Tethys in Indonesia and The Philippines. Proc. 5th Ann. Conv. Indon. Petrol. Assoc. 2, p. 25-52. Audley-Charles, M.G. (1978)- The Indonesian and Philippine archipelagoes. In: M. Moullade & A.E.M. Nairn (eds.) The Phanerozoic geology of the world, II, The Mesozoic. Elsevier, p. 165-207. Audley-Charles, M.G. (1981)- Geological history of the region of Wallace’s Line. In: T.C. Whitmore (ed.) Wallace’s Line and plate tectonics. Clarendon Press, Oxford, p. 5-25. Audley-Charles, M.G. & D.J. Carter (1974)- Petroleum prospects of the southern part of the Banda Arc, eastern Indonesia. Comm. Co-ord. Joint Prosp. Min. Res. Asian Offshore Areas (CCOP), Techn. Bull. 8, p. 55-70. (Mainly an overview of the geology of Timor, with some comments on oil seeps and prospectivity of island) Audley-Charles, M.G., D.J. Carter & A.J. Barber (1974)- Stratigraphic basis for tectonic interpretations of the Outer Banda Arc, Eastern Indonesia. Proc. 3rd Ann. Conv. Indon. Petrol. Assoc., p. 25-44. (Outer Banda Arc islands (Timor, Tanimbar, etc.) are imbricated N margin of Australian shelf and slope on which overthrust Asian elements and major olistostrome have been superimposed, all emplaced from N) Audley-Charles, M.G., D.J. Carter & J.S. Milsom (1972)- Tectonic development of Eastern Indonesia in relation to Gondwanaland dispersal. Nature Phys. Sci. 239, p. 35-39. Audley-Charles, M.G. & R. Harris (1990)- Allochtonous terranes of the Southwest Pacific and Indonesia. Philos. Trans. Royal Soc. London A331, p. 571-587. (Mainly on Timor. Deformed Australian margin, overridden by three allochtonous nappes) Audley-Charles, M.G. & D.A. Hooijer (1973)- Relation of Pleistocene migrations of pygmy stegodonts to island arc tectonics in eastern Indonesia. Nature 241, p. 197-198. (Pleistocene pygmy stegodonts in Sulawesi, Flores and Timor, areas now separated by deep seas. Dwarf Stegodon co-existed in Flores and Timor in Pleistocene. Flores now separated from Timor by 3,000 m deep Savu Sea, narrowest in Ombai Strait (30 km) between Alor and Timor. Because elephants (and presumably stegodonts) could not swim across Savu Sea- Ombai Strait, a Pleistocene land connection between Flores and Timor must be postulated (but elephantoids now believed to be rel. good swimmers; HvG) Badan Geologi (2009)- Sedimentary basins map of Indonesia based on gravity and geological data, 1:5000,000. Geol. Survey Indonesia, Bandung. (online at: www.grdc.esdm.go.id) (Map of Indonesia sedimentary basins, color-coded by age and labeled by basin type) Bibliography of Indonesian Geology v.4.1 7 www.vangorselslist.com July 2012 E Miocene (P22/N3. S. Bangkok 2008. 204. In: D. ('The Paleogene in the Indies Archipelago'.1 8 www.chula.Oceans. H. Assoc.Eurasia collision in Taiwan) Barr. 11.com July 2012 . but severely criticized in series of papers by Van Bemmelen. Spec. Neubauer & A. Barber.E. Dev. p.vangorselslist. Earth Planets Space 52.Improving the velocity field in South and South-East Asia: the third round of GEODYSSEA. followed by uplift. Verhand. Michel & C. 8. N18.pdf) (Review of GEODYnamics of S and SE Asia (GEODYSSEA) project. G. R. Proc. D.. (Old seismic profiles and interpretation NW Australia. Rak & D. Am. 3-17.co. Major Late Pliocene. A.Late Miocene (N11/12N14/17). Francais Petrole 37.pdf) (W Burma-W Sumatra ribbon-continent has Cathaysian E Permian fauna and flora. (online at http://mail. P. p.Tectonic controls on magmatic-hydrothermal gold mineralization in the magmatic arcs of SE Asia. p. (3) majority and largest deposits formed since 5 Ma during plate reorganization with change in relative motion between Indian-Australian and Pacific plates between 5. & A.Dispersion. Publ. R. Barber. Bin Nordin. 39-47. p. starting with major transgression at MiocenePliocene boundary. 233-292.N10-11.N7?.The origin and emplacement of the West Burma-West Sumatra ribboncontinent. Angermann.Oligocene). (Five main depositional cycles in Eocene. Symp. 508-512. observed between 1994-1998) Bibliography of Indonesian Geology v. 1. Bull. p.uplift?. volcanism. 721-726. In Miocene two blocks separated by formation of Andaman Sea) Barber. M. S. Geol.E Oligocene (P11-P17). (IAGI).Het Palaeogeen in den Indischen Archipel.J. Koolhoven. E. p. Reinhart. (Most gold deposits in SE Asian arcs formed during tectonic reorganization intervals rather than steady-state subduction: (1) 25 Ma collision of Australian craton with Philippine Sea plate arc.Recent of Java. Soc. 3.M. Amer. Overview of Paleogene sediments in Indonesia and Philippines.. (1993). Proc. Hall & E. Conv.5 Ma following Philippine arc. & S. Useful compilation. etc. (3) late E Miocene. Reigber (2000). Forde (1994).) (1981). A. Geoscience Resources and Environments of Asian Terranes (GREAT 2008). CCOP-IOC Working Group Meeting.Geology and jungle fieldwork in Eastern Indonesia. p. Centre. F. 23. a network of 42 GPS stations across SE Asia.4. Assoc. & P. 18-23.Badings. Wiryosujono (eds. Geology Today 10. Bull. (2) Latest Oligocene. P.H.jp/journals/EPS/pdf/5210/52100721. Publ. Gen. ending with volcanism. Lehner (1975). new frontiers in exploration.geo. Geol.ac. 2. Separated in M-Late Permian from E margin of Cathaysia as thin continental sliver by formation of a backarc basin and by M Triassic had moved along transcurrent fault system around Indochina into present position W of Sibumasu. 415 p. Geol. Geol. subduction and collision in Eastern Indonesia. (2) M Miocene/ 17 Ma mineralization following maximum extrusion of Indochina and cessation S China Sea spreading. Nederland en Kol. 1. poorly known). Sumatra: (1) M Eocene. Baumann. MacDonald (1981). Res.J. 4th IGCP 516 and 5th APSEG. b. p.J. p.J. Blundell.Recent volcanic phase) Beck. Crow (2008). 92.Geochemistry and geochronology of Late Cenozoic basalts of Southeast Asia: summary.. London. 18-21. Petrol. in 1936) Baker..M Miocene (N8. In: Proc Int. (Conference volume with many benchmark papers on tectonics of Eastern Indonesia) Barley.th/Geology/English/News/Technique/GREAT_2008/PDF/001. M. 58. (4) M.The geology and tectonics of Eastern Indonesia. 22nd Ann. Soc. similar to S China and Vietnam. Wyman (2002). With outcrop distribution/ basic paleogeographic maps for Tertiary a. 376-395.3. c and d (Eocene. (5) Pliocene-Recent.H. followed by uplift. Spec. Ubaghs.sc.. (online at: http://www. Geol. Indon. Geol. faulting.Depositional cycles on magmatic and back arcs: an example from Western Indonesia. Geol. block faulting.Sunda Arc) Becker. von Avadt (eds. A. Mijnbouwk. S. Bandung 1979.S.) The timing and location of major ore deposits in an evolving orogen.J. (1982). Ser. (1936). Revue Inst. & M.terrapub. 1. but still interesting discussion of Australia. 93-97. J.The timing and location of major ore deposits in an evolving orogen.The evolution of marginal basins and adjacent shelves in east and Southeast Asia.Cenozoic basin formation in Southeast Asia.E Indonesia paleogeography) Benson. Royal Soc. S Banda Arc (CW rotation rel.Orogenesis and deep crustal structure. 16p. Beltz. Soc. 39-47. to Sunda and Australia). sect.Geologische Probleme im Malayischen Archipel. NW Australia. (1978). Y.P. Benioff. Genrich. J. (1939). H. 385-400. p..) Berlage.Principal sedimentary basins in the East Indies.J. Trans. Lee (1993). Tectonophysics 45. now called ‘Benioff zone’) Benson. (Sunda arc example of dipping earthquake zones below volcanic arcs. New Zealand 55. (1954). without own synthesis or opinion) Blundell. McCaffrey. L. 204. F. 1440-1454.J.N. Z. p. Neubauer & A. H. Bijlaard. (Old. 62.P. the geodynamic context. C. diepzeetroggen. 65. 135-138. L.Structural framework of the Sunda Shelf and vicinity. geosynclinalen. I. (First text to notice deep earthquakes in Indonesia are on plane dipping toward Asian mainland (now known as Benioff zone) Berlage.De verklaring voor het optreden van zwaartekracht anomalieen.) The timing and location of major ore deposits in an evolving orogen. Blundell. 71p. Bock. Royal Soc. etc. 108. but still interesting discussion of tectonics. (Old. Ben-Avraham. 19181936. Technology/ Woods Hole. 2367. (2002). L. (1936). von Quadt (eds. Z. J. Jena. mountain building and volcanism near local plastic deformation of the earth’s crust’) Blom. De Ingenieur in Nederl.Y.D. Geol. Spec. Progress Rept. Prawirodirdjo. In: D.N. C.A. p. p. Subarya et al. p. California. geosynclines. D. subducting beneath Seram Trough) and E Sulawesi (CW rotation. AAPG Bull. p. p. Proc.. 7-17. 17p.Beckley.Crustal motion in Indonesia from Global Positioning System measurements. Crustal blocks all experience significant internal deformation). of Texas.. (1937). ('Geological problems in the Malayan Archipelago'. Gerland Beitr. Inaugural-Dissertation Friedrich Schiller University. transferring E-W Pacific motion into N-S shortening across N Sulawesi trench. (1934). Austin. W. Bull. p. 269p.One hundred deep-focus earthquakes in the Netherlands Indies.W.A provisional catalogue of deep-focus earthquakes in the Netherlands East Indies. Ph. Trans.. P. Geophys. Res. 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Banda Arc used as example) ESCAP (1976). Report of 1910 geographic expedition to Bali. No correlation with age of subducting ocean floor or thermal parameters of slab) Ernst. (Depth to top subducting slab below Java volcanoes ~100km. Regional Working Group. USA 94. Lombok. Kuntjara (1990). (Broad overview of Indonesia mineral resource assessment) Edelman. Dev. Geol. Int. UHP paragneisses contain most abundantly preserved crustal diamonds.. Wetar. Engdahl & W. Worldwide ranges 65-130 km. Kabaena.A geologic and mineral resource assessment of Indonesia. D. 4432-4460. (1999). Singapore 1998. Leidsche Geol. Amsterdam. 5. Sci. Proc. Assoc. transcurrent faults and internal deformation adjacent to southeast Asia and western Pacific. Deepwater and Frontier Exploration in Asia & Australia Symposium. 77. Res.J.Philippine region. 7p. (1972). Geophys. (2).F. (1933). Asia. James & R. J.. Holmes (1995). p. Sci. Possible explanation involves delamination within continental crust. 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Gen. 727-740. 50.Subduction of continental lithosphere in the Banda Sea region: combining evidence from full waveform tomography and isotope ratios. Jakarta. Kon. (1998). SEAPEX meeting. Seismol. Martin commerative volume. Indon.1 18 www. In: R. Nederl. Nederl.com July 2012 .Deep water exploration off Southeast Asia. T. J. Rev. Earth Planet. p. 1431-1444. 677-685. Somerton &G.Feestbundel uitgegeven ter eere van Prof. J.4. Res. 748p.A new global satellite gravity dataset for screening and evaluating offshore basins in S. BGS Technical Report.Shallow seismic reflection profiles from the waters of east and southeast Asia: an interpretation manual and atlas.G..nl/DL/publications/PU00016465. B. Tijdschr. Estimates of temperature lowering in Late Pleistocene strikingly greater in mountains than in lowlands) Bibliography of Indonesian Geology v.H. (‘On the indirect relationship between volcanism and Vening Meinesz’ belt of negative gravity anomalies in E Indies’) Escher.Over het indirecte verband tusschen het vulkanisme in Ned. Martin 1851-1931.C. Umbgrove & P. Meded. Soc. Late Jurassic ocean lithosphere N of N Australian craton was capable of entraining large volumes of continental lithosphere. B. 6.Escher. Petrol. p. In the 1950's/ 1960's these understood to be expressions of Benioff/ subduction zones) Escher. Fichtner. M. (In montane areas in Sunda-Sahul region Upper Montane rainforest appears to be absent in Late Pleistocene. Kuenen (1931). I.Focal mechanisms along inclined earthquake zones in the Indonesia. van Bergen (2010). p.H.Plate convergence. (1933). p.vangorselslist. Akad. (eds.J.E.R.W. C. separating upper from lower crustal units. (1970). T. J.M. Dr..pdf) (Pre-plate tectonics paper exploring the apparent relationships between belts of active volcanoes.) Proc. Wetensch. DFE04-PO-006. Flenley.On the relation between the volcanic activity in the Netherlands East Indies and the belt of negative gravity anomalies discovered by Vening Meinesz. A. Noble et al. p. R. Lett. dipping zone of earthquakes and zone of negative gravity anomalies as recently identified by Vening Meinesz. B. with evidence from Pb isotopes for lower-crust involvement in arc volcanism) Fitch.dwc. C.-Indie en de strook van negatieve anomalie van Vening Meinesz.Earthquake mechanisms and island arc tectonics in the Indonesian-Philippine region. America 60.G. (online at: http://www. 15. p. With listings of species and fossil localities and stratigraphy) Evans. I. suggesting mantle-driven dynamic topography.S. S. 124-147. & M. suggesting negative dynamic topography and heatflow anomalies due to basin formation above slab burial grounds) Garwin. 25. S. I: Text. (Gold and copper deposits in SE Asia and W Pacific largely in M-L Cenozoic (25–1 Ma) magmatic arcs. R. G. Hydrothermal systems active for durations of <100.. II: Enclosures. Negative anomalous depth of several back-arc basins is ~650-800 m (range 300-1100 m). & D. Gage. vol.4. In: D.E. 891-930. p. Hall & Y. p. Indon. p. Garwin. Y.Accretion of the southern Banda Arc to the Australian plate margin determined by global positioning system measurements. 9.1 19 www. another 35 remains to be found.Fletcher. Several major tectonic events N of Australia at ~45 Ma. Most of Australia. Digital Geoscience Map Series G-2.dipping subduction. de Smet (1991). 83.Southeast Asian basin-types versus oil opportunities. basins and hydrocarbon plays) Fugro-Robertson (2008).J. Vol. Three major plate reorganizations at ~45. wrench and suturerelated basins) Gaina C. (Reconstruction of tectonics and depth history of Indonesian seaway and associated SE Asian back-arc basins. MacDonald (ed. (1996). 100th Anniv.Indonesia's Tertiary basins.dipping subduction zone. Over 35 billion bbl oil found. and 5 Ma.. Conv.. 177-203.) Sedimentation. M. and Solomon Sea (42-33 Ma) S of S. Multiclient study.Eurasia convergence appears to occur as N-ward translation of Banda Arc. SEAPEX 1976. with Caroline (37-24 Ma) and Celebes Seas (48-35 Ma) opening N of N. A. A. Publ.Digital geologic map of East and Southeast Asia. Geol. 9th Ann. London. Conference. 79-89. Matthews & R.the land of plenty. p.J.I. Assoc.Cenozoic tectonic and depth/age evolution of the Indonesian gateway and associated back-arc basins.com July 2012 .A. L. (Genetic classification of 63 SE Asia basins. 1-27. Paper 8. Tomography shows marginal basins with negative dynamic topography underlain by massive buried slab material. 12. with shortening on Flores and Wetar thrusts) Geological Survey of Japan (2004). Fraser.000.000 years) Genrich. 288-295.R. Ann. p.M. E.F. p. Keynote Papers.L.Exploration opportunity screening: Eastern Indonesia-Papua New Guinea. accompanied by negative regional heatflow anomalies. p. 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Petroleum Systems of SE Asia and Australasia.Paleogene basin development in Sundaland and it's role to the petroleum systems in Western Indonesia. 47. 562-566.. Stille & F.-Phys. p.The geology of the Netherlands Indies. Lotze (eds. Central Sunda slab penetrates lower mantle to 1500 km. p. (1992). & M.) (2003). S. Malaysia 9.G.. Aziz. Suharsono & S. 253-271. R. SE and S Sulawesi.Updating of Indonesian Tertiary basin sedimentary basins.Predicting sediment yields from SE Asia: a GIS approach. Cambridge Univ. Bandung 1987) ('New thoughts on the origin of geological terranes in Indonesia'. IAGI) 12 (Katili volume). Bangai-Sula. & R. 16th Ann. p. 6. 32nd Ann. Centre. London. etc. (Atlas of geology and potential of minerals and energy in Indonesia) Sukamto.. Bull. p. Porphyry copper. 345-357. Rept. 376384. R. Res.E. 1. R.Y. Res. Early mining from epithermal lode deposits hosted by volcanics in W Sumatra and W Java. (19 papers in English. T. In: G. Conv.) The Jurassic of the Circum-Pacific. Bandung. Inst. 107-123. p. (Summary of Jurassic stratigraphy and ammonites in Irian Jaya. Centre. S. Dev. & T. (Volcanic and non-volcanic arcs in NE Indonesia different types of metallic mineral belts) Sukamto.. p.M. UN ESCAP. Sukamto. Soc. Conv.) and on Flores-Wetar. Moores & R. Westermann (1992). mineral concentrations and hydrocarbon accumulations in the ESCAP Region series.Suhanda (1977). Kalimantan and Sulawesi) Suzuki . (Gold mining in Indonesia began in 1899. Press. Setyogroho. 181-193. Example of use of gravity data in S Kalimantan to determine basin outlines: propose to combine Pembuang and Barito basins) Sunarya. R.Indonesia and Papua New Guinea. Muyuo. Y. Kalimantan. with subsequent discoveries in Kalimantan (Kelian.associated gold in Ertsberg (Irian Jaya). Indon. Geol. B. Geol. (1989). Hokuriku Geol. Indon. 29th Ann. Assoc..G. Dev. scale 1: 10. Seram. Bibliography of Indonesian Geology v. Possibly tied to intense precipitation/ runoff and many areas of recent rapid uplift) Sukamto. N Sulawesi and Bacan. Wicaksono.Gagasan baru tentang asal berbagai mintakat geologi di Indonesia. & G. mostly on tectonic history and volcanism) Suggate. Indon. Geol. (LEMIGAS (2007) basins map lists 63 Tertiary sedimentary basins in Indonesia. IPA03-G-015. Hall (2003). Purbo-Hadiwidjoyo (1997).) (1989).vangorselslist.E. & Sidarto (1990). 16p. Misool. R.1 59 www. etc. 12 p. Sriwijaya..W. In: Epithermal gold in Asia and the Pacific.The Jurassic rocks in Indonesia. Geol. Chapman and Hall. Sumatra.4.000. Timor-Rotti. Atmawinata. Brief overview of terranes) Sukamto. (also in Proc. Proc. H. Assoc. Geologi Indonesia 12. A. Obi. S. p. Geol. Assoc.J. R. Munadi & B. 14.D. Petrol.Regional geology of Indonesia. (Overview of the 17 regions in Indonesia with Jurassic rocks in outcrop) Sukamto. Bandung. Borneo. Waigeo. Dev.C. Mt Muro. 1-14. Katili Commemorative Volume (60 years). Geol. Jamal. (Same paper as below) Sunarya.Buton.M. Mtg IAGI. Tjia et al. p.000. (1993).On the formation of Southeast Asia island arcs..Some notes on magmatic activities and metallic mineral occurrences in northeastern Indonesia.A. Wiyanto (2008). p. Westermann (ed. 1. produce very high volumes of sediments relative to size of its landmasses. Amin & D.com July 2012 . Centre 14. 635 p. Alluvial gold exploited on Sumatra. 155-161.Atlas geologi dan potensi sumberdaya mineral dan energi kawasan Indonesia. 5 in Indonesian. Buru. Indonesia (J. D.Overview of gold exploration and exploitation in Indonesia. 59-72. In: E. (Areas of Indonesia like New Guinea.Sudradjat. Tanimbar-Babar. Bull. Bull.. Proc. S. Petrol. B.) Encyclopedia of European and Asian regional geology. p. (eds. Res. 3. Andi-Mangga (1990). IPA08-G-163. Y. B.Overview of gold exploration and exploitation in Indonesia. Sumatra and PNG) Sunarjanto. Sukarna (eds. Fairbridge (eds. 4. Assoc. (1986). LeDain & R. K. 1.Propagating extrusion tectonics in Asia: new insights from simple experiments with plasticine. Largest along-strike variation in Java. Manila.1 60 www. (Depth to top of subducting slab below volcanoes 72. Tectonophysics 329.Terrestrial heat flow map of Indonesian Basins. New York. Peltzer. CCOP Techn. p. p. 39-60. but correlations exist between depth and slab dip. In: S. Geosyst.V. 95-116. & G. Armijo (1982). J. (Geothermal data from 929 wells in 20 Tertiary basins. 611-616.vangorselslist. Dominant change is shift in location of volcanoes in relation to slab and trench. Thamrin.M. J. Netherlands and Netherlands Indies Council of the Institute of Pacific Relations. and slab depths once again become near 100 km.Heat flow study in the oil basinal areas in Indonesia. p. Mey (1987). Prayitno & Siswoyo (1984). O'Brien (2000). D. Assoc.D.com July 2012 . and (2) cessation of most normal faulting in Late Miocene-Early Pliocene on seismic) Tapponier. 435444. (Using vegetation anomalies on satellite imagery to target nickel laterites) Taylor.Effective elastic thickness of the northern continental lithosphere subducting beneath the Banda orogen (Indonesia): inelastic failure at the start of continental subduction. New York.Terrestrial heat flow map of Indonesian Basins. (Pliocene-Recent Australian continent.Mining in the Netherlands East Indies.SE Sumatra to 150 km to E. 4. Evidence for inelastic yielding of N Australian continental lithosphere near presentday shelf-slope at continental subduction: (1) maximum change of EET near shelf-slope in laterally variable EET calculations. Thamrin. Jump at overlapping of ends of two volcanic lines. Not clear what causes this shift) Tandon. Ishihara.. 5. p. 8. volcanoes step back toward trench. p. in map and cross-section.. p. 45-62.Global compilation of variations in slab depth beneath arc volcanoes and implications. Joint ASCOPE/ CCOP Workshops I and II.Syracuse E. & S. Takenouchi (eds..Y. 1-110. TP 15.An investigation of the relationship between the geology of Indonesian sedimentary basins and heat flow density. Bull. Carter (1978). M. global average 105 km. Bibliography of Indonesian Geology v. 1977 reprint) (Overview of mineral deposits in Indonesia as known during WW-II) Thamrin. changing over ~150 km along strike. Skeenan & W. Depths correlate poorly with most subduction parameters. 33-70.. M. 18p. Spec. Tectonophysics 121. Indonesian Petrol. Ter Braake. C.Asia collision in Eocene) Taranik. A. Salawati Basin and Bintuni Basin may be caused by shallow magmatic diapirism) Thamrin. C.W. Proc. Change in Effective Elastic Thickness (EET) at start of continental subduction at Mio. A. Lorenzo & G. 49-60. Collision most advanced near C Timor. Thermal conductivity increases with depth of burial and compaction. (Popular. Geology 10. E of 119° E (W Banda Sea).173 km.Targeting exploration for nickel laterites in Indonesia with Landsat data.) Granitic magmatism and related mineralisation. G.Heat flow study in the oil basinal areas in Indonesia..H. Thamrin. Australian continental lithosphere N of Timor detached from oceanic lithosphere. 12th Symposium of Remote Sensing. M.A. van Leeuwen (1980). p. Geochem.A. Issue.Pliocene boundary due to change in curvature of N Australian lithosphere near shelf-slope. Petrol. where depth shifts by 70 km on either side of 108° E from 90 km in W Java. (1985). T gradient controlled by depth and T of heat source beneath basin.D.M.arc collision from Roti to Kai created underfilled foreland basin in Timor-Tanimbar-Aru Trough. Environmental Research Institute of Michigan.. & T.Porphyry-type deposits in Southeast Asia. S Sumatra. Geophys. (1944). 70 p... (also as Arno Press.M. Abers (2006). M. 1037-1051. Proc. Indon.L. High heat-flow densities in C Sumatra. p. & P. Mining Geology. p. (1985). but still disputed tectonic model explaining major strike slip zones and blocks rotations in SE Asia as results of India. 7. Reynolds. P. Publ. M. (2001)-Wrench tectonics in Sundaland. (1991). J. In: G. 165-185. collision) and intraplate sources of stress such as topography and basin geometry) Tjia. Tjia. (1968). Tjia. Widespread condensed oceanic sediments with Late Jurassic macrofossils overlie them. Tjia. p. Geophys. Geol. Bull.D. Tjia. (Variable stress pattern throughout SE Asia largely inconsistent with Sunda plate ESE motion direction. Irian FZ (1300km). Tectonophysics 482. Present-day maximum horizontal stress in Thailand. Union and Geol. 89-104. 2. H. R. Hall (2010). Vulcan.D. subsurface and offshore evidence. Hilde & S.Volcanic lineaments in the Indonesian island arcs. AAPG Bull. p. Late Cretaceous 'couches rouges' facies rich in calcareous plankton. Mesozoic on Buru. America Geodyn. (1973). asphalt. Geol. p. 11. In: N. Soc. p. Techn..) Proc. Geodin. S and C Sumatra basins maximum horizontal stress NE–SW. Milsom & D.D. Mijnbouw 52. Thiramongkol (ed. H. Geol. Maximum horizontal stress in Borneo primarily NW– SE. subduction forces (trench suction.) The geology and tectonics of Eastern Indonesia.D. 71-77. AAPG Int. Bandung. Inst. Proc. Res. may reflect plate-boundary forces or topographic stresses exerted by C Borneo highlands. active volcanoes and extensive limestone terrains (caving)) Tjia. This sequence may be preceded by basaltic volcanic phase.Present-day stress field of Southeast Asia. (1978). H. E Sulawesi and plateaus off NW Australian Shelf. Bandung. M.W. Geol. Magm. Uyeda (eds. Centre. 101-118.Active tectonics in the Indonesian Archipelago-2. those from Banda Arc mixed Austral-Tethyan elements.182. Banyumas Depression of Java. Conv. Morley.. central depression of Timor.1 61 www. H. Teh et al. 281-300.D. H. Ser.. 69.) Geological Society of Malaysia Ann. Malaysia. Bibliography of Indonesian Geology v. Bull. p.g. 1. (1983). Spec. Tjia. (eds. H. 9. 84. deposited in subtropical environment) Tingay.D. H.Philippines. Malaysia 42. Palu-Koro FZ. Assoc. Soc. Workshop on Correlation of Quaternary Successions in South. & J.Thurow. East and Southeast Asia.D. Plate-scale stress field in SE Asia controlled by combination of Himalayan-related deformation. First Eurasian microfauna in Maastrichtian. Amer. p. Buton. (IAGI). Sediments represent rifting off NW Australia.Mesozoic tectono-sedimentary evolution of the Banda Arc area.J. R.Active faults in Indonesia. (1989). Wiryosujono (eds. Conf. perpendicular to Indo-Australian subduction front. 10. Indon. Tjia. Seram. p. some with oil. Pacific Geol. D. (Abstract only. Hillis. (1968). Dept. Soc. Triassic sandstone and platform carbonates/ black shales).D. 413-422.New evidence of recent diastrophism in East Indonesia. Publ. H. 71-76. 92-104. 20th Ann. Geol. Bandung. E Cretaceous sediments pelagic with abundant radiolaria. Precollision sediments record complicated rift-drift-history from higher latitudes at NW Australian margin and include source and reservoir rocks (e. Dev. 2001.Earthquake stress directions in the Indonesian Archipelago. (1998). p.Active tectonics in the Indonesian Archipelago. indicating beginning of collision.Indonesia.Examples of young tectonism in Eastern Indonesia. p.4.H. 1505-1506. Geol. 175. Coblentz & R. Geol.C.D.com July 2012 . King. Roques (2000). H.) Geodynamics of the western Pacific-Indonesian region. (1981). C. (Main known active faults in Indonesia: Sumatra Fault Zone (1600 km). p. consistent with radiating stress patterns from E Himalayan syntaxis. Mesozoic pelagic microfaunas of NW-Australia typical Austral affinities (high latitude). Tjia. Sulawesi (700km). Tjia. Conf. Barber & S. Bangkok. In: A. Contr. 74-92. Vietnam and Malay Basin predominately N-S.Meridian-parallel faults and Tertiary basins of Sundaland. oil seeps. In: T. 21-30.D.Displacement patterns of strike-slip faults in Malaysia. H.. p. p.vangorselslist. Principal stress directions from wrench patterns. H. Umbgrove..H.The general geological survey of Block 2.younger sediments >12 km thick. In: P. Res. 2. p. K. Aardrijksk.A. Trail.K. Sugimura & T. J. 6. 106. Similarities suggest open sea connections in M Eocene. Abiong. Part 1.F. Proc.) Proc. Mining Metallurgy 10. possibly post-Miocene).H. 641-651. J. 769-834.C.4–2. p. Some N-striking wrench faults indications of up to 45 km right-lateral displacement. London.B. p. Cessation of spreading in Philippine Sea and Caroline basins by M Miocene changed wrenching into transpression. SE Asia (GEOSEA III). and some faunal interchange of fauna in Oligocene and later) Umbgrove. IIA. Indonesia and Malaysia.The occurrence and mining of gold in the Dutch East Indies.C. 33-43. 487-495. S. Bangkok. & Wiryosujono (1978). (Unpublished but widely used report) Truscott S.V. Parwoto & Subagio (1974). Obial.vangorselslist. 6. 68 p. (Four radiocarbon dates of elevated strandlines in tectonically active areas of E Indonesia and E Malaysia indicate uplift rates between 4. 1. Soc. Fujii. 427-433. (1930). Geol. 49. Nederl. Sugimura & T.Tertiary sea-connections between Europe and the Indo-Pacific area. (On similarities and differences between Indo-Pacific and European Tertiary faunas. Discussion of Tertiary basins) Bibliography of Indonesian Geology v.D.J. Regional tensional conditions prevailed until E Miocene. Nutulaya (ed.Kigoshi.Changes in tectonic stress field in northern Sunda Shelf basin. Geol. S. accompanied by slip-sense reversals and structural inversion) Tjia. (Tertiary basins of N Sunda Shelf are underlain by normal and attenuated continental crust. D.Ophiolites in eastern Indonesia. 52-86. In M. other basins between 4-8 km. 4. Kigoshi.4. T.D. Special Publ. 31 p. J.D. Third Reg. Quaternary Res. A. (1932). Gen. With map showing 11 Neogene tectostratigraphic regions A-M) Umbgrove. Neogene sediments highly variable in thickness and intensity and timing of deformation. Towards margins stress trajectories deviate due to convergence of adjoining megaplates and SE extrusion of Indosinia. (Review of Neogene stratigraphy in Indonesian Archipelago. forming pull-apart depressions and modifying structure of large depocentres. p.S. K.Late Quaternary uplift in Eastern Indonesia. (Radiocarbon dates of 15 samples from raised shorelines on various islands of E Indonesia suggest rates of tectonic uplift up to 12. Tectonophysics 23.9 mm/ year during past 24.5 mm/year) Tjia. Leidsche Geol. H. p. and inversion of basin-filling sediments.Hall & D.F.com July 2012 . p. In Malay basin. Liew (1996). Date from S arm of Sulawesi indicates rate of uplift of 1. regional compression caused reversals on wrench faults. one of regionally common shorelines at 2 m above sea level dated at 2590 ± 100 yr BP) Tjia. Min.. In: R. Oligocene. 291-306. 4.. Trans. Fujii. Petzel. M.H. Until onset of M Miocene most wrenching transtensional.5. S. W Malaysia. & K. Zakaria (1972). H.F. (1933). Zakaria (1974). B. Conf.Radiocarbon dates of elevated shorelines. (‘Different types of Tertiary geosynclines in the Indies Archipelago’.(Wrenching widespread in Sundaland. well-bore breakouts and major earthquakes show most of Sundaland currently subjected to N-S stress. R. A. Bird. Tjokrosapoetro. Inst. Java 1929. Sulawesi Utara. Tijdschr. with comments on 163 areas. Meded. Kon. 91-104.000 yr. p. At Langkawi islands. D. John. PT Tropic Endeavour Indonesia Report. Blundell (eds.Late Miocene.) Tectonic Evolution of Southeast Asia.1 62 www. (1902). Fourth Pacific Science Congress.5 mm/ year.Het Neogeen in den Indischen Archipel. characterized by moderate-high geothermal gradients >5°C/100 m. no connection in Late Eocene.Verschillende typen van Tertiaire geosynclinalen in den Indischen archipel. 4p.4. Delft. Kawakatsu (2006). p. (1935). (‘Timing and types of Tertiary folding in the zone of negative gravity anomalies in the Indies Archipelago’. & B.Geological history of the East Indies. 163-182. 33.H.1 63 www.On the time of origin of the submarine relief in the East Indies.. 7. volcanoes. Aardrijksk. 2. Gulf Publishing. (1950). 51. p. 1. Lett. VIII.H. J. Barlow (1981).vangorselslist.F. (‘On the origin of the Indies Archipelago’) Umbgrove. Ned. J. p.Oil fields. p. 18th Int. Gen.Structural history of the East Indies. Ned. 1-70.The origin of deep-sea troughs in the East Indies. J. Res. Untung. (1935). (Concise overview of Indonesian seas.De Pretertiaire historie van den Indischen Archipel. Bandung. II.Tijd en type der tertiaire plooiingen binnen de zone van sterk negatieve afwijkingen der zwaartekracht in den Indischen archipel. structural zones and a series of broad paleogeographic maps) Umbgrove. AAPG Bull. Tijdschr. (Classic overview of geologic evolution Indonesian archipelago) Umbgrove. (1949). 119155. 53-63.J. Niu & H.Umbgrove.Over het ontstaan van den Indischen Archipel. & A. 22.A short survey of theories on the origin of the East Indian Archipelago. Tijdschrift Kon.) Vacquier. C. Honolulu 1990.H. (1934). Congr. (1948). V. Geol. (1938). J. (1938). M. J. (1996). 163-183. Review of Paleozoic-Mesozoic rocks in Indonesian Archipelago. Publ. Houston. Amsterdam 1938. 20-34. 8. p. (Data from nine deep earthquakes confirmed existence of mid-mantle discontinuity beneath Java arc and also revealed its presence N to Kalimantan.R. Umbgrove. Spec.Geoscientific study along Jawa-Kalimantan-Sarawak-South China Sea transect.1029/2005GL025106.H. Waltman. (Short critical overview of more than two dozen theories on origin of Indonesian archipelago published since late 1800's) Umbgrove. Untung. 63p. Geol. L04302. Kon. J. Res. Conf. 81-98.H. M. Geol. p. Congress. p. J. 52. (Strong E-W trending gravity gradient along N coast Irian Jaya. Barber & S. Wiryusujono (eds.F.The gravity field of Eastern Indonesia.F.C. E.. J. Press.) The geology and tectonics of East Indonesia.H.H. p. Int. Cambridge Univ. (Pre-plate tectonic attempt at explaining origin of deep sea trenches by 'downbuckling of crust') Umbgrove.. 5th Circum-Pacific Energy and Mineral Res. doi:10. see Van Bemmelen 1949) Umbgrove. deep sea basins.H. Geoph. Aardrijksk. Congr. Great Britain.F. In: A. Great Britain.F. With information of Tanimbar stratigraphy from unpublished work by Weber.Observations of the mid-mantle discontinuity beneath Indonesia from S to P converted waveforms. Dev.F. II.) Trans. Int. (1984).. Geogr. In: F.a source of heat flow data. Chapter 7. 2. p. Salisbury (eds. Gen. F. 73-80. 150-159. Vening Meinesz (1934).Gravity expeditions at sea 1923-1932.F. With small distribution maps and map/ table showing grouping in 7 Mesozoic tectonostratigraphic units A-G) Umbgrove.H. S to P waves converted at discontinuity at depth range ~1080 km in W to ~930 km in E) Bibliography of Indonesian Geology v.The origin of deep sea troughs in the East Indies (with discussion).F. Meded.A.F. Leidsche Geol. In: G.com July 2012 . p. with values decreasing from 130 mW/m2 in C Sumatra to 70 mW/m2 in E Kalimantan) Vanacore. Tectonophysics 103. (1934). J. p. Centre. (Heat flows somewhat elevated in Tertiary basins of W Indonesia. 1. 17-24. 73-80.P. 18th Sess. ('The Pre-Tertiary history of the Indies Archipelago'.C. etc. Van Bemmelen, R.W. (1931)- De bicausaliteit der bodembewegingen. Natuurk. Tijdschrift Nederl.-Indie 91, 3, p. 363-413. ('The double causes of ground movements'. First unveiling of Van Bemmelen’s ‘undation theory’, a tectonic theory that is a variation of the oscillation-theory of Haarmann and never found much acceptance. Crystallization processes in upper mantle trigger uplift ('geotumors'), subsidence and outward flows to reestablish hydrostatic equilibrium) Van Bemmelen, R.W. (1932)- De undatie-theorie (hare afleiding en toepassing op het westelijk deel van de Soenda boog). Natuurk. Tijdschrift Nederl. Indie 92, 1, p. 85-242. (Van Bemmelen’s ‘undation theory’ and its application to the W part of the Sunda orogenic arc). Van Bemmelen, R.W. (1932)- Nadere toelichting der undatie-theorie. Natuurk. Tijdschrift Nederl.-Indie 92, 2, p. 373-402. ('Clarifying comments on the undation-theory'. Reply to critical comments of Van Tuyn & Westerveld (1932)) Van Bemmelen, R.W. (1933)- Versuch einer geotektonischen Analyse Sudostasiens nach der Undationstheorie. Proc. Kon. Nederl. Akad. Wetensch., Amsterdam, 36, 7, p. 730-739. (online at: http://www.dwc.knaw.nl/DL/publications/PU00016473.pdf) ('Attempt at a geotectonic analysis of SE Asia after the undation theory'. Possibly historically interesting, but otherwise very controversial interpretation of SE Asia tectonics) Van Bemmelen, R.W. (1933)- Versuch einer geotektonischen Analyse Australiens und des Sudwestpazifik nach der Undationstheorie. Proc. Kon. Nederl. Akad. Wetensch., Amsterdam, 36, 7, p. 740-749. (online at: http://www.dwc.knaw.nl/DL/publications/PU00016473.pdf) ('Attempt at a geotectonic analysis of Australia and the SW Pacific after the undation theory'. Possibly historically interesting, but otherwise very controversial interpretation of Australia-Pacific tectonics) Van Bemmelen, R.W. (1933)- Die Neogene Struktur des Malaysischen Archipels nach der Undationstheorie. Proc. Kon. Nederl. Akad. Wetensch., Amsterdam, 36, 10, p. 888-897. (online at: http://www.dwc.knaw.nl/DL/publications/PU00016473.pdf) (‘The Neogene structure of the Malay Archipelago after the undation theory’. Possibly historically interesting, but otherwise very controversial interpretation of Indonesia tectonics) Van Bemmelen, R.W. (1935)- Over het karakter der jongteriaire ertsgangen in den vulkanischen binnenboog van het Soenda systeem.. Geol. Mijnbouw 14, p. 21-25. ('On the nature of the young Tertiary ore veins in the volcanic inner arc of the Sunda system') Van Bemmelen, R.W. (1935)- Uber die Deutung der Schwerkraft-Anomalien in Niederlandisch Indien. Geol. Rundschau 26, 3, p. 199-226. (‘On the significance of the gravity anomalies in the Netherlands Indies’. Belt of negative gravity anomalies identified by Vening Meinesz and explained by him as downwarping/ buckling of light sialic crust thought to be better explained with Van Bemmelen’s ‘undation theory’) Van Bemmelen, R.W. (1938)- On the origin of the Pacific magma types in the volcanic inner arc of the Soenda Mountain System. De Ingen. in Nederl. Indie 5, 1, p. Van Bemmelen, R.W. (1938)- The distribution of the regional isostatic anomalies in the Malayan Archipelago. De Ingen. in Nederl. Indie, ser. IV, 5, 4, p. 61-67. Van Bemmelen, R.W. (1939)- Gravitational tectogenesis in the Soenda Mountain System. 17th Int. Geol. Congress, Moscow 1937, 2, p. 361-382. Bibliography of Indonesian Geology v.4.1 64 www.vangorselslist.com July 2012 Van Bemmelen, R.W. (1940)- Bauxiet in Nederlandsch-Indië. Dienst Mijnbouw Nederl.-Indie, Verslagen en Mededeelingen betreffende Indische delfstoffen en hare toepassingen 23, 115 p. ('Bauxite in Netherlands Indies'. Lateritic weathering of probably basic igneous rocks lead to the formation of bauxite. Occurences in Netherlands Indies on Banka, Bintan, ) Van Bemmelen, R.W. (1941)- Origin and mining of bauxite in Netherlands Indie. Econ. Geol. 36, 6, p. 630640. Van Bemmelen, R.W. (1949)- The geology of Indonesia. Government Printing Office, Martinus Nijhoff, The Hague, vol. 1, Geology, 732 p. (also 1970 reprint with updated references list) (Classic overview of pre-WWII knowledge of Indonesia geology. Still the most comprehensive compilation of geology of region. Excellent documentation of the state of knowledge of regional geology and stratigraphy of Indonesia at the end of the colonial period. Tectonic interpretations using the 'undation theory' model are controversial and outdated) Van Bemmelen, R.W. (1949)- The geology of Indonesia. Government Printing Office, Martinus Nijhoff, The Hague, vol. 2, Economic geology, 265p. Van Bemmelen, R.W. (1949)- The geology of Indonesia. Government Printing Office, Martinus Nijhoff, The Hague, vol. 3, Plates. Van Bemmelen, R.W. (1950)- On the origin of igneous rocks in Indonesia. Geol. Mijnbouw 12, 7, p. 207-220. Van Bemmelen, R.W. (1950)- Gravitational tectogenesis in Indonesia. Geol. Mijnbouw 12, 12, p. 351-361. (Only vertical movements are result of endogenic forces. All other tectonic forces are reactions to gravitation) Van Bemmelen, R.W. (1952)- De geologische geschiedenis van Indonesie. Van Stockum, Den Haag, 139 p. (‘The geological history of Indonesia’. Popular summary of Indonesia geological evolution) Van Bemmelen, R.W. (1953)- Relations entre le volcanisme et la tectogenese en Indonesie. Bull.Volc., ser. II, 13, p. 57-62. (‘Relations between volcanism and tectonics in Indonesia’) Van Bemmelen, R.W. (1954)- Mountain building; a study primarily based on Indonesia region of the world’s most active deformations. Martinus Nijhoff, The Hague, 177 p. (Pre-plate tectonics text book on mountain building, primarily based on Indonesian geology. Interpreted mainly in terms of Van Bemmelen's controversial and outdated 'undation theory') Van Bemmelen, R.W. (1955)- L’evolution orogenetique de la Sonde (Indonesie). Bull. Soc. Belge Geol. Pal. Hydr. 64, 1, p. 124-152. (‘The orogenetic evolution of Indonesia’. Another overview of Indonesia tectonic evolution in terms of the preplate-tectonic ‘undation theory’) Van Bemmelen, R.W. (1961)- Volcanology and geology of ignimbrites in Indonesia, North Italy, and the USA. Geologie Mijnbouw 40, 12, 14 p. Van Bemmelen, R.W. (1965)- Mega-undations as the cause of continental drift. Geol. Mijnbouw 44, 9, p. 320333. Van Bemmelen, R.W. (1965)- The evolution of the Indian Ocean mega-undation (causing the Indico-fugal spreading of Gondwana fragments). Tectonophysics 2, 1, p. 29-57. Van Bemmelen, R.W. (1976)- Plate tectonics and the undation model. Tectonophysiscs 32, p. 145-182. Bibliography of Indonesian Geology v.4.1 65 www.vangorselslist.com July 2012 (Final paper on Van Bemmelen's undation theory' first proposed by him in 1931, but never found acceptance, especially after the advent of plate tectonics theory) Van der Voo, R. (1993)- Paleomagnetism of the Atlantic, Tethys and Iapetus Oceans. Cambridge Univ. Press, 411 p. (Review of global paleomagnetic data, including Sibumasu, Borneo, E Indonesia, etc.. Misool-Timor probably not continuously part of Australian Plate: Misool paleolatitudes 10-20° lower than predicted if remained with Australia. Large rotations suggested for Cretaceous of Sumba and Timor) Van Es, L.J.C. (1919)- De tectoniek van de westelijke helft van de Oost Indische Archipel. Jaarboek Mijnwezen Nederl. Oost Indie 46 (1917), Verhand. 2, p. 15-144. (‘The tectonics of the western half of the East Indies Archipelago’. Synthesis of Western Indonesia geology as known in 1917) Van Es, L.J.C. (1918)- De voorhistorische verhoudingen van land en zee in den Oost-Indischen Archipel, en de invloed daarvan op de verspreiding der diersoorten. Jaarboek Mijnwezen Nederl. Oost Indie 45 (1916), Verhand. 2, p. 255-304. ('The prehistoric relationships of land and sea in the East Indies Archipeago and its influence on the distribution of the animal species'. Pliocene paleogeography of Indonesian archipelago) Van Gool, M., W.J. Huson, R. Prawirasasra & T.R. Owen (1987)- Heat flow and seismic observations in the northwestern Banda Arc. J. Geophys. Res. 92, B3, p. 2581-2586. (High heat flow values in centers of three basins in NW Banda Arc. Average in N Buru basin 161 mW/m2. Two small, N-S to NW-SE elongated subbasins in Lucipara basin 175 and 134, mW/m2, respectively. High heat flow in N Buru and Lucipara basins interpreted to be result of recent E-W strike-slip movement in NW Banda Arc) Van Hinte, J.E., T.C.E. van Weering & A.R. Fortuin (eds.) (1989)- Proceedings of the Snellius II Symposium, Geology and geophysics of the Banda Arc and adjacent areas, Jakarta 1987, vol. 1. Netherlands J. Sea Res. 24, 2-3, p. 93-381. Van Hinte, J.E., T.C.E. van Weering & A.R. Fortuin (eds.) (1989)- Proceedings of the Snellius II Symposium, Geology and geophysics of the Banda Arc and adjacent areas, Jakarta 1987, vol.2. Netherlands J. Sea Res. 24, 4, p. 383-622. Van Leeuwen, T.M. (1994)- 25 years of mineral exploration and discovery in Indonesia. J. Geochem. Explor. 50, 1-3, p. 13-90. (History of mineral exploration by foreign companies in Indonesia between 1967 and 1991. Four main phases: (1): 1967-1976) mostly investigations of mineral prospects previously identified by Dutch; (2) (1970-1975) extensive porphyry copper search in Sunda arc, W Sulawesi and central belt of Irian Jaya; (3) (1981-1988) extensive coal exploration in S and E Kalimantan; (4) (1984-1990) major gold rush, focused primarily on Cenozoic magmatic belts of Kalimantan, Sulawesi, Moluccas and Sunda arc) Van Tuyn, J. & J. Westerveld (1931)- Opmerkingen naar aanleiding der 'undatie theorie' van Bemmelen en hare toepassing op het westelijk deel van de Soendaboog. Natuurk. Tijdschr. Ned. Indie 92, p. 341-372. (Critical review of Van Bemmelen’s new tectonic 'undation theory' and its application to the western part of the Sunda Arc) Vening Meinesz, F.A. (1930)- Maritime gravity survey in the Netherlands East Indies, tentative interpretation of provisional results. Proc. Kon. Nederl. Akad. Wetensch., Amsterdam, 33, p. 566-577. (online at: http://www.dwc.knaw.nl/DL/publications/PU00015922.pdf) (First account of Vening Meinesz' well-known shipboard gravity work. Principal feature discovered is a ~100 miles wide narrow strip of strong negative anomalies through whole archipelago (W of Sumatra, S of Java, islands of Timor, Tanimbar, Kei, Seram, then to North), bordered at both sides by fields of positive anomalies. With map of ship traverses and stations, and axis of negative gravity anomalies) Bibliography of Indonesian Geology v.4.1 66 www.vangorselslist.com July 2012 Proc. Geologische verkenningstochten in het oostelijke gedeelte van den Nederlandsch Oostindische Archipel.a geophysical study. Verbeek.go. Extra bijvoegsel Javasche Courant 1900. F. p. Includes brief paleontological reports by specialist paleontologists. Tijdschr. possibly also on Ambon and Babar. 66. Early summary of Verbeek (1908) book) Verbeek.A. Geol.Th. M. F. R. + Atlas. The expeditions. Delft. Soc. 8. Nederl. Geol. Netherlands Netherlands Geodetic Commision. Vol. Gen. (French edition of Verbeek (1908)) Vergnolle. Bull. Akad. ('Preliminary account of a geological trip through the eastern part of the Indies Archipelago'. Batavia. 453-457.Deep focus and intermediate earthquakes in the East Indies. 56. Aardrijksk.M. Kuenen (1934).Indonesian archipelago. 197-207. F. B11403. America 65. (Early paper on belts of strong negative gravity anomalies and the theory of ‘crustal downbuckling’ (which came close to recognizing subduction)) Vening Meinesz.nl/DL/publications/PU00017410. (online at: http://www.. F. Calais & L.F.4. Kon. Government Printing Office. (1932). 855-865. (1940). Amsterdam 43.dwc. The interpretation of the results. widespread. H.M. J. (1900). Kon.com July 2012 .M.H. (2010). J.. p. Permian present on Timor and adjacent islands. Proc. (1908).De theorie van Wegener. R.D.A. Kon.Molukkenverslag. F. the computations and the results.Rapport sur les Moluques. etc. (1954). 826p.Gravity expeditions at sea 1923-1932.nl/DL/publications/PU00015922. Ged. and last of Verbek's voluminous reports on geology of parts of Indonesia.Indonesian landforms and plate tectonics. (1946). I. II.dwc.geological reconnaissance trips in the eastern part of the Netherlands East Indies archipelago’. (online at: http://www. (Another model of Asia tectonic plates relative horizontal motions from GPS measurements) Verstappen. 'Old schist formation' metamorphics rel. p. Amsterdam 49.The earth's crust deformation in the East Indies.id/publication/index. Akad. Delft. J.knaw. Vening Meinesz.knaw.A. R. Nederl.. Wet. Res. p. H. F. Wetensch. 3-48. Indonesia 5. 143-164.D. Widespread marine Mesozoic sediments.1 67 www. Wetensch. (online at: http://www. p. Comm. 112.A.php/dir/article_detail/275) Bibliography of Indonesian Geology v. Umbgrove & Ph. p. 3..A. 3. Waltman. geology and morphology of the East Indian archipelago. (1908). Netherlands Geol.A. Oost-Indie 37 (1908).D. 844 p. p. Ed. Geophys. Shift of axis of Sunda-Banda trench minimum gravity zone between Sumba and Timor) Vening Meinesz. Gravity.bgl. 278-293.pdf) (New regional isostatic gravity anomaly map of Indonesia. 109-194. TriassicJurassic rocks and faunas similarities with Himalyas and Alps.Voorlopig verslag over eene geologische reis door het oostelijk gedeelte van den Indischen Archipel. + Atlas (‘Moluccas Report. Classic early geological reconnaissance survey of 250 islands in E Indonesia.Dynamics of continental deformation in Asia.Gravity expeditions at sea 1923-1932. 1-22. Nederl.vangorselslist.pdf) Vening Meinesz.. Dong (2007). Jaarboek Mijnwezen Nederl.Vening Meinesz. Vol. p. ) Verbeek.esdm. (Geophysical work in Netherlands Indies and other regions no clear data to support or negate the Wegener theory of continental drift) Vening Meinesz. (1939). Reconnaissances geologiques dan la partie orientale de l'archipel des Indes orientales neerlandaises. E. 5. Batavia. Ser. C. 120 p. Sitzungsber. Visser. p. Timor and Kolonodale blocks detached from Gondwana in Jurassic. C. C.Geodynamic evolution of Eastern Indonesia from the Eocene to the Pliocene. Timor and Kolonodale joined Eurasian margin by end Paleogene. Honthaas & C. Bellier. Australian and Pacific plates: (1) Banda (= dismembered E Sulawesi. Geophysik 53. Living and raised coral reefs. (3) Lucipara (S Banda Ridges. M. Buru. Main events: (1) Late Eocene-Oligocene collision Banda block. Cornee. (Abstract). 84. (1930).. Monnier (2010). Earth Plan. Rehault. p. with E Miocene metamorphism event) and (4) Halmahera.Sulawesi. Tukang Besi). J. (1937). Magnet. p. Seram and Bangga-Sula detached from PNG in Neogene. suffered opening of N and S Banda back-arc basins by Late Miocene. Lucipara.M Pliocene and. M. Electr. Tanimbar. (5) Late Pliocene collisions of Australia and Banda and Irian Jaya blocks. p.J. And Atm. 1153-1167. Magn. S. Timor and Kolonodale (or Argo) blocks came from NW Australian margin. P.W.J.P. Rehault.The main steps of the geodynamic evolution of Eastern Indonesia since Upper Eocene times.K. 18. Tukang-Besi Ridge + Kur.1 68 www. (2000).A connection between deep-focus earthquakes and anomalies of terrestrial magmatism and gravity. 9. with Kolonodale.Der Malaiische Archipel. Lucipara. (1938). (2) BanggaiSula. 264-275. Conf. Biogeography 27. Erlangen 44. AAPG Bull. Compt.J. Seram and Banggai-Sula collided with Sulawesi between M Miocene. Kon. (2) E Miocene collision Lucipara Block (incl. J. river systems and time durations. 178-204. Sinta Ridge).vangorselslist. S. H. Oligocene-E Miocene arc. Soz. Timor block moved S with S margin of S Banda basin and collided with N Australian margin in M Pliocene) Villeneuve. Seram. J. p. Sci. volcanoes. Phys. Cornee. Geobanda-Group (1998). 361-362. C. (2000).P. O. en Meteor. 7 blocks (six from NE Gondwanan margin. Gerlands Beitr. J. Paris. p. J. All Gondwanan blocks collided with Eurasian active margin near Sulawesi. Terr. Observ.. W. 420-437..W. AAPG Int. Hinschberger. 19021926. S. J. J. Visser. In: The geodynamics of S and SE Asia (GEODYSSEA) Project. Volz. and fault scarps are important geomorphic indicators of active plate tectonics) Villeneuve.E Sulawesi. Banda. Gunawan. Visser. Burhannuddin. Indo-Australian. R. 1511.W. F. Gondwana Res. Seram and Banggai-Sula blocks originated from W extension of PNG while Irian Jaya block is still linked to N Australian margin. (1912). (Rather simplistic series of maps from Australia to Sri Lanka to Taiwan showing areas of exposed land in IndoAustralian region during periods of Pleistocene when sea levels were below present day levels) Bibliography of Indonesian Geology v. (E Indonesia 3 main plates (Eurasian.(Landforms in Indonesia resulted primarily from plate tectonics. (3) Late Miocene extension with opening of N. Honthaas & W. Cornee. M. J. Bali 2000. Verhand. 5. (Geodynamic reconstruction based on evolution of 4 continental blocks.On the distribution of earthquakes in the Netherlands East Indian Archipelago II. (4) E Pliocene collision Banggai Sula. obsolete tectonic model of Indonesia) Voris.Banda Block in Buton.Deciphering of six blocks of Gondwanan origin within Eastern Indonesia (South East Asia). Greatest relief amplitudes near plate boundaries: deep ocean trenches at subduction zones and mountain ranges at collision belts.4. Early.Mediz.com July 2012 . H. ('The Malay Archipelago: its framework and relation with Asia'. Banda.P. 42.Maps of Pleistocene sea levels in Southeast Asia: shorelines. IIA. Savu basins. Villeneuve..Seismic isobaths in the East Indian Archipelago. Gunawan (1998). Timor with its Late Miocene calc-alkaline intrusions in N was part of Banda Arc before M Pliocene collision with Australia) Villeneuve. sein Bau und sein Zusammenhang mit Asien. Rehault.Tectonostratigraphy of the East Indonesian blocks. p. Rehault. Cornee. Halmahera from Pacific plate). S. Albrecht. 291-302. Bellon. 327. p. J. 22. Honthaas. Acad Sci. M. Rend. trapped by convergence of Asian. W. Honthaas et al. Weltevreden. 389391. Philippine-Pacific). Lucipara. S. 4. Martini. J. 106. (Cretaceous mélange in C Java (Luk Ulo). S Sulawesi.Coord. Forde (1996). Publ.. (http://www. 1. Metals and Fuels 52. Malaysia Bull. J. Hall & D. ultramafic rocks. (1997). limestone (ridge covered by reefs). K.vsi. Stratigraphy and tectonic evolution in Southeast Asia and the South Pacific and IGCP 359 and IGCP 383.) Tectonic Evolution of Southeast Asia. formation of volcanic islands near ridge covered by reefs.sandstone (sedimentation at or near trench of convergent margin).esdm. P. Asian Earth Sci. Metcalfe (2005).Oceanic plate stratigraphy and tectonics in East and Southeast Asia. 679-702. (Pb-Nd isotope signatures of igneous and (meta) sedimentary rocks from E Indonesia continental fragments help identify provenance areas: Ambon-Seram= southern New Guinea. Banda Ridges = ‘Pacific’ New Guinea and Sumba= Sundaland) VSI (Volcanological Survey Indonesia) (2005). J. 739-749.4. radiolarian chert (pelagic sediment). (2000). pelagic deposition of radiolarians on oceanic plate. S and C Sulawesi and S Kalimantan(Meratus. (1999). Teh (ed. 32nd Ann. Radiolarian biostratigraphy shows oceanic plate subduction occurred continuously along paleo-trench during Cretaceous) Wakita. 24. 201-218. Sess. accretion and collison along the southeastern margin of Sundaland. Van Bergen & E. radiolarian chert and melange. C Java (Karangsambung. mixing with detrital clays to form hemipelagic siliceous shale.html) Wahju. In: G. E and SE Asia (CCOP). Collision exhumed very high pressure metamorphic rocks from deeper part of accretionary wedge) Wakita.Current status of mining in Indonesia.Cretaceous accretionary: collision complexes in central Indonesia. carrying microcontinents detached from Gondwanaland. Conf. p.H. Int. radiolarian chert and shale. (1996).) Proc. Coastal Offshore Geosc. and deposition of sandstone. Bacan= North Australia. Typical ‘Ocean Plate Stratigraphy’ (OPS) from old to young: pillow basalt (birth of oceanic plate at mid-ocean ridge).Vroon. p. Survey Indon. p. Accretionary wedge with fragments of oceanic crust. p.Ocean plate stratigraphy in East and Southeast Asia. Laut) reflect Cretaceous convergent SE margin of Sundaland craton. & I.Geothermal resources in Indonesia.) Proc. Progr. glaucophane schist. (Early version of Wakita series of papers on Cretaceous accretionary complexes at SE Sundaland margin. (2004). Mines. with special reference to Jurassic melanges of Japan. Volc. with immature volcanic arc at periphery. (eds. Geol.) Proc. 6. 19-30. 388-401. Dheeradilok et al. Tsukuba 1995. Soc. p. calcilutite sedimentation at flank of volcanic islands. In: S. p. (VSI) Geothermal Division. (Components of ancient accretionary complexes include pillow basalt. Radiolarian biostratigraphy provides information on time and duration of ocean plate subduction) Bibliography of Indonesian Geology v. 445-453. Blundell (eds. Lithologic successions in different tectonic units similar and reflect ‘Oceanic Plate Stratigraphy’ sequence: birth of oceanic plate at oceanic ridge. Geol.N.vangorselslist. This margin surrounded by marginal sea. 158-166. In: P. K.Cretaceous subduction.Pb and Nd isotope constraints on the provenance of tectonically dispersed continental fragments in East Indonesia. B.Z. Bangkok.Mesozoic melange formation in Indonesia. K. limestone. Asian Earth Sci. siliceous shale (mixed radiolarians and detrital grains in hemipelagic setting) and shale. M. Kim et al. K. (Cretaceous accretionary complexes in W Java (Ciletuh). Wakita.shale near trench of convergent margin. In: R. (eds. 43. etc. p. K. Jiwo). P. Oceanic plate subducted beneath arc from S.1 69 www. J. Common blocks of metamorphic and ultrabasic rocks derived from blocks exhumed following microcontinent collision) Wakita. particularly Luk-Ulo melange complex in C Java and Bantimala Complex of S Sulawesi) Wakita.go. (Ancient accretionary wedges recognized by glaucophane schist. Kuala Lumpur.. London.J. Comm. as shown in example of Luk-Ulo Melange of C Java.com July 2012 . p. Soc. GEOSEA '98.Y.id/pbumi/index.J. S Sulawesi (Bantimala) and S Kalimantan (Meratus) mainly polymict clasts in muddy matrix. 18. Radiolarian biostratigraphy useful for reconstruction of accretionary complexes. Jurassic shallow marine allochthonous formation was emplaced by collision of continental blocks in Bantimala. Spec. Verh.. nebst Bemerkungen uber Orbulinaria Rhumbler und andere verwandte Foraminiferen. HvG)) Bibliography of Indonesian Geology v. J. Miyazaki. 75-99. 5. A. 567-609. Geol. (1931). p.N.Einige geologische Ergebnisse einer im Jahre 1909 ausgefuhrten Reise durch den Ostlichen Teil des indoaustralischen Archipels: Vorlaufige Mitteilung. Leidsche Geol.Zur Tektonik der Molukken.Mesozoikum In: B. Xie (2001). Y. Marker species for latest Jurassic (+earliest Cretaceous? (NB: these are not foraminifera. 436-460. (Early paper on the tectonics of the Moluccas) Wanner.G.vangorselslist. (’Triassic fossils from the Moluccas and Timor Archipelago’. Meded. Escher et al. 155-165. (eds. Pal. Meded. From Misool. C Java.H. Pal. Roti. p.Echinodermata In: B.. Japan 48. Zhang & G..) De palaeontologie en stratigraphie van Nederlandsch Oost-Indie. Palaeont. Pal. Mijnb. 1910. p. Lett. J. 22. 2. 137-147. Martin memorial volume). Ser. I. Earth Planet. 736-741. Leidsche Geol. p. ocean plate subduction followed by collision of continental fragment) Waluyo (1992). 569-599. (1921).. J.. p. M. Buton and E Sulawesi. but different histories. (Review of distribution of Mesozoic rocks in E Indonesia. 3-5. (1907).) may be lenses in flysch section. First description of Upper Jurassic calcispheres Stomiosphaera moluccana and Cadosina fusca from Timor. S Sulawesi. Geol. etc. Zeitschr. Massive U Triassic limestones of E Seram (with solitary coral species Montlivaltia molukkana n. Yin.sp. J.G. Kol. Mem. J. ('News on the Permian. Triassic and Jurassic formations of the Indo. T. Luk-Ulo. Geosciences J. ('Some geological results of a 1909 trip through the eastern part of the Indo-Australian Archipelago') Wanner. Geol. Timor. Geol.D. Seram. also product of oceanic plate subduction in island arc setting. (1940). J. Bantimala. Wanner.Seismotectonics of eastern Indonesian region.H. S. Overview of Triassic faunas of Misool. p. Zulkarnain.Digital terrane map of East and Southeast Asia..) Wanner. Nederl. Rel. Roti. (1910). (‘Rock-building foraminifera from the Malm and Lower Cretaceous in the eastern East Indies Archipelago’. (1910). Geol.Triaspetrefakten der Molukken und des Timorarchipels. Wang. Neues Jahrbuch Miner. K. Trias.Gesteinsbildende Foraminiferen aus dem Malm und Unterkreide des ostlichen Ostindischen Archipels. 152-162. C.und Juraformation des Indo-Australischen Archipels. 188. 161-220. Ph. 22. Sci.Neues uber die Perm-. p.) De palaeontologie en stratigraphie van Nederlandsch Oost-Indie. (‘The Malayan geosyncline in the Mesozoic’. 123-133. p.Wakita. 4. K. Escher et al. common on E Seram. Misool. J. Seram. (eds. subduction complex formed by continuous subduction of oceanic plate throughout Cretaceous. I. (Listings of fossil echinodermata described from Indonesia) Wanner. K. Soc. J. J. Metcalfe. Geol. Grove. Centralblatt Miner. Bd. 343 p. p. (1931). Wakita. Martin memorial volume). Timor) Wanner. (Sundaland surrounded by accretionary complexes and accreted microcontinents rifted from Gondwanaland. Daigo (2000).1 70 www.Thesis St.A tectonic model for Cenozoic igneous activities in the eastern Indo-Asian collision zone. Louis University. 5 (K. 8 (Verbeek volume). Beil. Centralblatt Miner. Borneo.Die Malaiische Geosynklinale im Mesozoikum. 5 (K. Sopaheluwakan. Harrison. S Kalimantan. detailed review of Mesozoic stratigraphy and macrofaunas across Indonesia) Wanner. Savu. J.Australian Archipelago') Wanner.Q. (1925). Rundschau 12. Meratus. p. Cretaceous accretionary complexes in C Java.M.4. Daonella spp. Hada & M. Sumatra.J.com July 2012 . Geol. Roti. ’Alpine’ mollusc Monotis salinaria and brachiopod Halorella spp. 19-22.. 24. p. S Sulawesi and S Kalimantan similar components.Cretaceous subduction complexes along the southeastern margin of Sundaland. Gen. Parkinson & Munasri (1997). ) Tin-granites end-stages of differentiation of acid magmas. ('The origin of the continents and oceans'.com July 2012 .The granites of the Malayan tin belt compared with tin-granites from other regions. (2) Gold-silver mineralization on Sumatra. Malaysia. connecting W Borneo with E Burma through Malaya. p.tin-bearing biotite-granites) Westerveld. Annal. Geol. 1199-1209. Classic book on continental drift theory. Repts. etc. Kon. Int. Bull. J. with Au-Ag-bearing base metals in Sumatra. Sect. & N. Nederl. J.Permian brachiopod correlations for South-East Asia. etc.or.Die Entstehung der Kontinente und Ozeanen. p. Early Cretaceous deep sea sediment formed ~1000 km to S. (online at: http://www. associated with ultrabasic rocks) Westerveld.vangorselslist. Suggate. Indonesia Tin Islands. Amsterdam. J.Fasen van gebergtevorming en ertsprovincies in Nederlands Oost-Indie.A. English version of above paper) Wheeler. Braunschweig. (Abbreviated.Waterhouse. I. (1987). Soc. 10. 1.4. Congr. (1922). In: Proc. ('Metal provinces in the Netherlands East Indies'. etc. S.. (Summary of paleomag data. J.id/fosi/ ) (Brief review of ongoing Indonesia research projects at University of London/ Royal Holloway group) Wegener. J. Berita Sedimentologi 23. associated with ?Cretaceous intrusives. with epithermal Au-Ag-and Mn-ores.nl/DL/publications/PU00016993.1 71 www. ('Phases of mountain building and ore provinces in Netherlands East Indies'. Malaysia. (Absence of measurable dynamic topography in SE Asia) Bibliography of Indonesian Geology v.knaw. Geology of Southeast Asia.SE Borneo). 39. Burma. Vietnam. Wetensch. (2) Cretaceous Sumatra orogen (Sumatra-Java. Proc. I.. Geology 28.M. 1-25. 30p. Thailand. Geol. (3) W and S Sumatra gold-silver associated with post-Miocene intrusives and (4) nickel-iron in Banda Arc.Displaced terranes of Gondwana origin in Indonesia: paleomagnetic implications. (1973). Hall. P. Sevastjanova.E Sulawesi.dwc. 18th Sess. 6. 187-210. du Nord VII. (1949). iron laterites and diamond-gold placers in Borneo (3) M Miocene Sunda orogen from W Burma through inner Sunda islands to W arc of Sulawesi.B. p. A. Amsterdam.Quest for dynamic topography: observations from Southeast Asia. p. Four main metallogenic provinces: (1) tin islands BangkaBillition. 11. Gunawan et al. W of New Guinea four concentric orogens: (1) Late Jurassic Malaya orogen. gold and bauxite. Vieweg. (1952).Phases of mountain building and mineral provinces in the East Indies. 13. 963-966. (1939).New insights into the geological evolution of Eastern Indonesia from recent research projects by the SE Asia Research Group. 245-255. R. p. Original position of Misool rel. Explanation for arcuate shape of Banda Arc by NW movement of Australia. (1936). 3rd ed. (online at: http://www. Great Britain 1948. De Ingenieur 1949. shifted N with N drift of Australia). M. Good maps of ore deposits) Westerveld. Public address at the start of position of lecturer in economic geology at the University of Amsterdam. p. brachiopods and ammonoids) Watkinson. Soc. Cottam. Timor: Permian is displaced terrane of Australian origin. (4) Late Cretaceous.. H. with proportions of main constituents not essentially different from non. 21-27. I. (2012). (Correlations of Permian sections in Indonesia. p. to Australia was farther N than today) Westerveld. 81-87.Metaalprovincies in Nederlandsch Oost-Indie.pdf) (Great petrographic uniformity of tin-bearing and related granite rocks of Inner Malayan Arc (Malay PeninsuIa. 12-13. Geol. using fusulinids. with tin.iagi. Regional Conf.M Miocene Moluccas orogen through outer Sunda islands and E arm of Sulawesi. White (2000). 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P. indicating Cathaysian and Sibumasu biotas began to merge. 5-6. Res. M Permian Timorites. & E. different from both peri-Gondwanaland (no true E Permian glacial deposits) and Cathaysian biotas (no Permian coals).S. 375-385. p. & E. Palaeoclim. p. & A. Malaysia and Timor) Fan.Ammonite faunas and palaeobiogeography of the Himalayan belt during the Jurassic: initiation of a Late Jurassic austral ammonite fauna. Shi. 59. (2) No tropical Cathaysian biotas and reef complexes. incl. 4. Y. Fang. (2000).1 85 www. Equatorial Tethyan (incl. 134. J. Koloskov (2005). especially in E margin.W. Monie & S. Triassic intracontinental tectonics. (4) Common endemic genera and species) Fang. Ser..com July 2012 . Wang.. Cariou (1997). Ural and Boreal elements. p. Sinica 30. G. 829-848. leading previous authors to accept a Triassic age for NCB-SCB collision) Fedorov. Waagenoceras?) and Peri-Gondwanan (incl.Carboniferous and Permian zoogeographical change of the Baoshan Block. Himalayas. J. SW China. 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First period characterized by potassic basalt (Vietnam) and tholeiitic bimodal (SE China) volcanism. which was not single block.(Three main periods of activity in Cenozoic volcanic complexes of SE China. They signify pelagic basin at W side of Shan-Tai Terrane. E Permian Brachiopods fauna can be correlated with those of E Permian of Irian Jaya. due to Late Carboniferous. between Shan-Thai and Gondwana. incl. Micropal. Sukhothai Terrane. 777-785.. Ptaluctida and Spiriferida. Asian Earth Sci. but composed of Paleotethyan Ocean and two continental terranes affiliated to Gondwana and Cathysian domains respectively) Feng. Wonganan. in melange zone composed of Silurian to Triassic slices. which was not single block.L. Pamirs. similar similar to E Permian of W Australia. 346-365.M-Late Triassic radiolarians from ribbon chert in NW Thailand indicate pelagic basin in this region. C.. Q.vangorselslist. Thailand. . D. (Alternative model for Cambrian. NW Thailand. p. ‘Shan-Thai Block’ in N Thailand. 6. Differs in Palaeotethys suture location in Thailand at Mae Yuam fault. which detached from Indochina and S China during back-arc opening due to W-ward subduction of Palaeopacific.M. 2.An alternative plate tectonic model for the PalaeozoicEarly Mesozoic Palaeotethyan evolution of Southeast Asia (Northern Thailand-Burma). etc. 3. 24.. O. late Ladinian and M Carnian radiolarians (51 species) from Mae Hong Son. N. ) Feng.4. Tectonophysics 451. J. (Early Carboniferous. Ingavat-Helmcke & M. p.Early Carboniferous radiolarians from North-West Thailand: palaeogeographical implications. Pakistan Salt Range. Ingavat-Helmcke & B. Stampfli (2008). 84. representing Paleotethyan pelagic basin in Late Paleozoic-Triassic. Malila.Discovery of Australia Early Permian brachiopods Faunas from Bianping Section of Southwestern Guizhou Province. Ingavat-Helmcke (2004).. This also explains location of Cathaysian W Sumatra block W of Cimmerian Sibumasu block) Bibliography of Indonesian Geology v. Chonglakmani.. Q. C.China and it's significance. Globiella foordi. can be divided from E to W into Sukhothai.. Situated on ‘Shan-Thai Block’. p. K. p. p. Guizhou Geology 1998. Miocene and Pliocene-Quaternary. Science in China D. 47. R. C. Rev.Triassic geodynamic evolution of SE Asia. Q. 377-393. D.com July 2012 . (E Permian brachiopod fauna from Bianping section.L. Inthanon. Helmcke & R. 11131119. 12. This suggests Shan-Thai terrane had already rifted apart from Gondwana in E Carboniferous. but composed of Paleotethyan Ocean and two continental terranes affiliated with Gondwana and Cathaysian domains. (Yunnan. (middle Early Carboniferous radiolarians from bedded cherts S of Mae Hong Son. Faunas chiefly Asselian-Sakmarian. belongs to Cathaysian domain and suture corresponding to Changning-Menglian Suture in Yunnan must lie to W of Sukhothai Terrane in Thailand) Feng. including Lampang-Phrae Basin. earlier than commonly assumed) Feng.M. Caridroit (2005)Permian and Triassic radiolaria from Northwest Thailand: paleogeographical implications.Helmcke. Hochard & G. Q..Correlation of Triassic stratigraphy between the Simao and Lampang-Phrae Basins: implications for the tectonopaleogeography of Southeast Asia. Afghanistan. with Strophomenida. Closure of E Palaeotethys related to S-ward oceanic subduction that triggered E Neotethys opening as back-arc. S China. Spiriferella sp.Mae Sariang area. C. Liu (2004). U Triassic magmatism in E Vietnam and L-M Permian arc volcanites in W Sumatra. To explain Carboniferous-E Permian and Permo-Triassic arcs in Cambodia. Helmcke. Beauvais (1986). 137-146. 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NW Australian margin two older breakup events: (1) latest Carboniferous-earliest Permian: departure of Sibumasu block and E Cimmerian continent (Baoxan. London 143. p. Australasian Assoc.A.On the distribution of the Late Palaeozoic floras in Asia. (1975). Berning (2007). In: Geology and Palaeontology of Southeast Asia. which leads us to think breakup event was latest Triassic. 1. p.G. Cathaysian/ Sino-Malayan or Gigantopteris in SE) Harzhauser. Cottam & M. p. M. p.A. Geol.The tectonic evolution of the Northwest Shelf of Australia and southern Southeast Asia.Correlation of the structural belts in East and Southeast Asia. N. D. p. M. L. R. etc. 311-449 (online at: http://www. p. SE Asian vegetation during last glacial maximum (ca. p. 1-94. (Upper Jurassic bivalves in W Borneo part of East Asian Province with Philippines and Japan. Mem. In: P. In: Geology and Palaeontology of Southeast Asia..A. 29.rbgsyd.pdf) (Argo and Gascoyne Abyssal Plains off NW Australia are only preserved patches of Tethyan ocean floor. Heads. ('Late Variscan orogenesis and terranes in Southeast Asia') Henderson. (2002). University of Tokyo Press. Seram. (1991). terrane tectonics and ecology. (1984)-The orogenic evolution (Permian-Triassic) of central Thailand.vangorselslist. R. with reconstructions in 20 Myr increments. 149. Late Campanian and Maastrichtian) Bibliography of Indonesian Geology v. Mem. 29-38. 18. p.Sc. Assoc. C. (eds. microfauna. assuming symmetrical spreading. flora in Australia. and modified rainfall patterns. D.) Continent-ocean interactions within East Asian marginal seas.gov. J. In: T. Timor-Roti. cooler temperatures. 215-228. Ingavat-Helmcke & D.Regional patterns of biodiversity in New Guinea animals. Gaina (2004). Douglas. Thulborn (2000). 83-91. Implications on paleogeographic models for mainland SE Asia. 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(Tropical rain forest in SE Asia developed in extensive archipelago during past 65 My or more. with increase in extent of montane vegetation and savannah and decline in rain forest) Heine. (online at: http://www. Dettmann. 37-54. (1984). 343-356.S. (Reconstruction of E Tethys (Mesotethys and Neotethys) ocean basin for last 160 Myr. Crampton.S. Gottinger Arbeiten Geologie und Palaeontologie.) Geology and Palaeontology of Southeast Asia 25.Hashimoto. & T. Misool.org/people/christian/media/Heine_02_MScThesis_e-version.A synopsis of climatic and vegetational change in Southeast Asia.. Miocene rain forest extended further N (to S China and Japan). etc.R. 58. (2003).earthbyte.Jurassic marine bivalve faunas and biogeography in Southeast Asia. France. Meischner (1993).1 91 www. Wright et al.pdf) (Interesting paper discussing present-day plant distribution in SE Asia (mainly Erica. (eds. C. G. Palyn. p.. 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Geology of Southeast Asia and adjacent areas. p.E Permian glacial. have Permo-Carboniferous glaciomarine deposits. Borneo and S Sulawesi) as result of Australian Plate collision with SE Asia) Xiaochi. J. Mem. H. Late Carboniferous.5° CCW rotation with respect to S China Block. Wopfner. Asian Earth Sci.periglacial deposits followed by deglaciation in E Sakmarian. Between Late Cretaceous. Royal Soc. Palaeoworld 18. 293-301.C. p.Late Jurassic to Cretaceous red beds from the Peninsular Thailand: implications for collision tectonics. (Late Carboniferous. (2) TMS (Tengchong Block.R. Publ.M Triassic ‘Pangea stage’ similar trends across Gondwana. with closure of Changning-Menglian Belt) Wopfner. H.Triassic. Yokoyama. Y. B. (1999). which underwent clockwise rotation after Jurassic together with Shan-Thai and Indochina blocks.vangorselslist. Laurie (eds. London. (1998). Talent & J. p. Hanoi 1995. H. coldwater faunas and Glossopteris flora. Assoc.J.4. In: Proc. 401-404. Two facies realms (1) intracratonic rift (Cashmere.A comparison between Permo-Carboniferous sequences of the Baoshan Block and the Lhasa Block. Wu. J.. I. Docking started in Late Triassic. p. Stow & Z. 29. Wu.C.M Miocene area experienced up to 24. Glacial series of Baoshan Block rel. p.V.. A. J. and separated from Gondwana in Artinskian. thin and overlain by thick basalts and red beds (volcanic rift setting?). large graben structures started to develop between Africa and India and between India and Australia. Tectonophysics 242.a review. Proc. Wang (1995). G. Spreading of Neo-Tethys lead to separation of Cimmerian Blocks from Gondwana in late E Permian. Spec. J. A.Y. & B.C. Lhasa. with typical facies with coal measures and redbeds. C. Soc.A. & X. developed on pericontinental non-volcanic rift along N margin of Australia and pre-Permian New Guinea and separated slightly earlier than LBS) Wopfner.Gondwana origin of the Baoshan and Tengchong terranes of west Yunnan. Strzelecki Symposium Vol. H. 539. (1996).com July 2012 . D.A. Hanoi. 1995. Australian Pal. China. Otofuji (2011)Paleomagnetism of the Middle.. indicating Gondwana position at that time and part of Sibumasu tectonostratigraphic unit. B. (Paleomagnetic analyses of 33 sites in Jurassic-Cretaceous red sandstones in Peninsular Thailand suggest two opposite tectonic rotations in Trang area.R. China.Gondwana Terranes of southwest China and their connections to India and Australia. 5-6.547. 515 p. Fujihara. a segment of the major Cathaysian-Gondwana divide in Southeast Asia. Symp. part of large scale CCW rotation experienced by S Sundaland Block (incl. M. J. Xiaochi, J. (2002)- Permo-Carboniferous sequences of Gondwana affinity in Southwest China and their paleogeographic implications. J. Asian Earth Sci. 20, p. 633-646. Yamashita, I., A. Surinkum, Y. Wada, M. Fujihara, M. Yokoyama, H. Zaman & Y. Otofuji (2011)Paleomagnetism of the Middle-Late Jurassic to Cretaceous red beds from the Peninsular Thailand: implications for collision tectonics. J. Asian Earth Sci. 40, 3, p. 784-796. (Paleomagnetic data of Jurassic- Cretaceous red sandstones from Peninsular Thailand suggests two opposite tectonic rotations in Trang area. As part of Thai-Malay Peninsula underwent CW rotation after Jurassic together with Shan-Thai and Indochina blocks. Between Late Cretaceous and M Miocene, as part of S Sundaland Block, up to 24.5° ± 11° CCW rotation relative to South China Block. N boundary of CCW rotated zone between Trang area and Khorat Basin) Yan, C.Y. & L.W. Kroenke (1993)- A plate tectonic reconstruction of the SW Pacific 0-100 Ma. In: E.M. Maddox (ed.) Proc. Ocean Drilling Program, Sci. Res. 130, p. 697-709. Yan, J.X. & D. Liang (2005)- Early and Middle Permian paleoclimates of the Baoshan Block, western Yunnan, China: insight from carbonates. J. Asian Earth Sci. 24, 6, p. 753-764. (Baoshan Block of W Yunnan, SW China formed E part of Cimmerian Continent in Permian. E Permian formed under influence of Permo-Carboniferous glaciation. After E Permian rifting faunal elements of Gondwana affinity decreased, while those of Cathaysian affinity increased. Late Permian faunas exclusively Cathaysian. E Permian Dingjiazhai Fm carbonates characterized by warm-temperate bryozoan-echinoderm facies of heterozoan association, with no non-skeletal grains. Overlying Yongde and Shazipo Fm carbonates subtropicaltropical chloroforam facies of photozoan association, with common non-skeletal grains) Yan, J. & H. Yin (2000)- Paleoclimatic constraints for early Permian paleogeography of Eastern Tethys. In: H. Yin et al. (eds.) Permian-Triassic evolution of Tethys and Western Circum-Pacific, Developments in Palaeontology and Stratigraphy 18, Elsevier, p. 1-15. (Paleoclimate indicators used to distinguish major Asian blocks. Early Permian cooler climate areas with diamictites and Glossopteris flora, warm climates have fusulinid limestones, Gigantopteris floras, etc. Suggest N-ward movement in Permian of blocks like Sibumasu from S Hemisphere Gondwana to N Hemisphere Asia) Yan, Q,, Z, Wang, S, Liu, Q, Li, H, Zhang, T, Wang et al. (2005)- Opening of the Tethys in southwest China and its significance to the breakup of East Gondwanaland in late Paleozoic: evidence from SHRIMP U-Pb zircon analyses for the Garze ophiolite block. Chinese Sci. Bull. 20, 3, p. 256-264. (U-Pb zircon analyses of gabbro from Garze ophiolite block from Garze-Litang melange yielded mean age of 292 ±4 Ma, suggesting earliest Permian sea floor spreading/ age of opening of Tethys at East Gondwanaland) Yang, Z. & J. Besse (1993)- Paleomagnetic study of Permian and Mesozoic sedimentary rocks from Northern Thailand supports the extrusion model for Indochina. Earth Planet. Sci. Lett. 117, p. 525-552. (Paleomagnetic study of Jurassic- Cretaceous sediments on Khorat Plateausuggests 1500 ± 800 km of post-M Cretaceous left-lateral slip along Red River and Xian Shui He fault zones and 14 ± 7° CW rotation for Indochina block relative to S China block, in agreement with lateral extrusion model of Indochina during India-Asia collision. Additional data of Permian, U Triassic and Lw Jurassic suggest Indochina, Yunnan (S China), N China block and S China block probably in contact at least since Late Triassic) Yang, Z., V. Courtillot, J. Besse, X. Ma, L. Xing, S. Xu &d J. Zhang (1992)- Jurassic paleomagnetic constraints on the collision of the North and South China Blocks, Geophys. Res. Lett., 19, 6, p. 577-580. (S China Block underwent final accretion to N China Block in M Jurassic. Accretion of NCB to Siberia was not complete until late Jurassic and possibly even until E Cretaceous) Yang, Z., Z. Sun, T. Yang & J. Pei (2004)- A long connection (750-380 Ma) between South China and Australia: paleomagnetic constraints. Earth Planet. Sci. Lett. 220, p. 423-434. (Paleomagnetic study on M Cambrian in N Sichuan Basin (Yangtze Block). S China Block placed against NW Australia, correlating Grenville-age Jiangnan orogenic belt with Rudall belt of W Australia, and subsequently Bibliography of Indonesian Geology v.4.1 125 www.vangorselslist.com July 2012 Late Proterozoic Jiangnan and Officer/Adelaide rift systems. Paleobiogeographic evidence indicates this configuration might maintain by M Devonian) Yap, S. (2002)- On the distributional patterns of Southeast-East Asian freshwater fish and their history. J. Biogeography 29, 9, p. 1187-1199. Yin, An (2010)- Cenozoic tectonic evolution of Asia: a preliminary synthesis. Tectonophysics 488, p. 293-325. (Cenozoic tectonic evolution model of Asia, including lateral extrusion of SE Asia between 32- 17 Ma after India- Asia collision) Yin, Hongfu (1997)- Triassic biostratigraphy and palaeobiogeography of East Asia. In: J.M. Dickins (ed.) Late Palaeozoic and Early Mesozoic Circum-Pacific events and their global correlation, Cambridge Univ. Press, p. 168-185. (Timor Triassic classified as ‘Gondwanan Tethys’ facies, similar to Lhasa- W. Birma?; different from ‘IndiaGondwana’ and ‘Cathaysian-Tethys’. Misolia is element of subtropical ‘Gondwanan Tethys’. Gondwanan Tethys and Tropical Tethys merged in Late Triassic due to S-ward expansion of tropical-subtropical biota) Yin, Hongfu, J.M. Dickins et al. (eds.) (2000)- Permian-Triassic evolution of Tethys and Western CircumPacific. Developments in Palaeontology and Stratigraphy 18, Elsevier, 412 p. (Reviews of Permian-Triassic in mainland E Asia, New Zealand, etc.; little on Indonesia/ New Guinea) Yin, J. (2003)- Oxfordian (Jurassic) mayaitid (ammonite) dispersal in the Tibetan Himalaya as the first signal of the establishment of the Indo-Austral subrealm. Progress in Natural Science 13, 4, p. 282- 287. (Mid-Oxfordian ammonite-fauna in Lanongla area, Tibetan Himalaya, characterized by endemic epimayaitids. Distribution of mayaitids around E Gondwana can be regarded as first signal establishment of Indo-Austral Subrealm in Late Jurassic-Early Cretaceous) Zakharov, Y.D., A.M. Popov & A.S. Biakov (2008)- Late Permian to Middle Triassic palaeogeographic differentiation of key ammonoid groups: evidence from the former USSR. Polar Research 27, p. 441-468. (Incl. paleogeographic reconstructions with Late Permian- earliest Triassic (260- 247 Ma) distributions of ammonites in Paleotethys) Zammit, M. (2010)- A review of Australasian ichthyosaurs. Alcheringa 34, p. 281-292. (On ichthyosaur fossils from Australasian region: Mixosaurus from M Triassic of Timor; Shonisaurus from U Triassic of New Caledonia, Platypterygius, from Lower Cretaceous of Australia and New Zealand) Zhao, D., S. Maruyama & S. Omori (2007)- Mantle dynamics of Western Pacific and East Asia: insight from seismic tomography and mineral physics. Gondwana Res. 11, p. 120-131. (Tomography of E Asia, the location of double-sided subduction zone where old Pacific plate subducts from E, and Indo-Australia plate subducts from S) Zhao, J.M. & G.D. Zhou (1987)- Discovery of Lytvolasma fauna from western section of Eastern Kunlun Mountains. Acta Palaeontologica Sinica 1987, 4, p. (Lytvolasma late E Permian coral fauna from E Kunlun Mts, W Qinghai. Includes Pleramplexus, Wannerophyllum, Lytvolasma, Lophophyllidium wichmanni, Timorphyllum, etc. Coral fauna characterized by simple forms with no dissepiments, signifying cold-water fauna. Comparable to Basleo beds of Timor) Zhao, X., R.S. Coe, S.A. Gilder & G.M. Frost (1996)- Palaeomagnetic constraints on the palaeogeography of China: implications for Gondwanaland. Australian J. Earth Sci. 43, 6, p. 643- 672. Zhang, Y.C., L.R. Cheng & S.Z. Shen (2010)- Late Guadalupian (Middle Permian) fusuline fauna from the Xiala Formation in Xainza County, Central Tibet: implication of the rifting time of the Lhasa Block. J. Paleontology 84, 5 p. 955-973. Bibliography of Indonesian Geology v.4.1 126 www.vangorselslist.com July 2012 (Fusulinid fauna from Xiala Fm of Tibet 9 species dominated by Nankinella and Chusenella, indicating Midian (Late Guadalupian) age. Earliest record of fusulinids in Midian in Lhasa Block suggests it rifted later than Qiangtang Block to N and Baoshan -Tengchong blocks to E, which have earlier (Artinskian) fusuline faunas and drifted away from Gondwana to relatively warm temperate zone in M Permian) Zhang, K.J. (1998)- The Changning-Menglian suture zone: a segment of the major Cathaysia-Gondwana divide in Southeast Asia-comment. Tectonophysics, p. 319-321. Zhang, K.J. (2000)- Cretaceous palaeogeography of Tibet and adjacent areas (China): tectonic implications. Cretaceous Res. 21, p. 23-33. (During Cretaceous, Tibet and adjacent areas under influence of gradual transgression. In S Tibet major transgression during Late Barremian-Albian, with thick inner shelf limestone in N Lhasa, suggesting back-arc extension during late Early Cretaceous) Zharkov, M.A. & N.M. Chumakov (2001)- Paleogeography and sedimentation settings during Permian- Triassic reorganizations in biosphere. Stratigraphy Geol. Correl. 9, 4, p. 340-363. (Artinskian- Kungurian Metaperrinites and Kungurian Perrinites faunas in Ratburi Group in N Central and S Central Thailand, represent part of Tethyan perrinitid belt from Crimea in W to Timor in E) Zhu, D.C., Z.D. Zhao, Y. Niu, Y. Dilek & X.X. Mo (2011)- Lhasa terrane in southern Tibet came from Australia. Geology 39, p. 727-730. (Detrital zircons from Paleozoic metasedimentary rocks in Lhasa terrane (Tibet) have distinctive age population of ~1170 Ma withHf values identical to coeval detrital zircons from W Australia. Those from W Qiangtang and Tethyan Himalaya terranes age population of ~950 Ma. The ~1170 Ma detrital zircons in Lhasa terrane were most likely derived from Albany-Fraser belt in SW Australia. Lhasa terrane is exotic to Tibetan Plateau and should be placed at NW margin of Australia) Ziegler, A.M., M.L. Hulver, A.L. Lottes & W.F. Schmachtenberg (1997)- Permian world topography and climate. In: I.P. Martini (ed.) Late glacial and post-glacial environmental changes- Quaternary, CarboniferousPermian and Proterozoic, Oxford Univ. Press, p. 111-146. Ziegler, A.M., P.M. Rees, D.B. Rowley, A. Bekker, L. Qing & M.L. 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Indonesia: primitive Sunda Arc magmas in an extensional tectonic setting? J. 1643-1683. Horizontal beds of sulfur in E part of crater wall of Idjen volcano. Gertisser (2008). biotite-leucite tephrites. Bull. Pyle (2001). 100.M. Kol. Persistently active between 1799-1898) Carn. S. J. 95. M. Java. J Volcanol. M. are crater lake deposits) Chadwick. GeoJournal 28.J.oxfordjournals. Abundant xenoliths. lavas include medium-K basalts and basaltic andesites. 4.full. Verhand. Geothermal Res.P. Volc. Geol.knaw. J. Indonesia). Bronto (1996). 971-982.Vincent (2000). E of Flores. Java. R. Gertisser. Camus..The Lamongan volcanic field. Indonesia. Camus. (Lamongan volcanic field in SE Java 61 basaltic cinder or spatter cones. 81-108. Petrol. & R.A.Het zwavelvoorkomen van de Kawah Idjen. p. Nederl. Waight & J. III (Molengraaff issue). Gloaguen. Geotherm. Troll. Indonesia): an outline of the structural and magmatological evolution. V. A. etc.A. Carey. M.com July 2012 . 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Mijnbouwk. 299-316. Vincent (1992). Sedimentology 58. p.vangorselslist. Ginibre.Merapi (Central Java. along with high-K suite. E Java. p. J.E. p. 139-163. 9. E Java.R. D. & D.. probably responsible for this and other features of complex) Caron.4. A.. complexly zoned. Sr isotopes require source or melt with elevated radiogenic Sr. Geol. The least evolved lavas lowest SiO2 contents (43 wt % SiO2) in Sunda arc volcanics.pdf) (Batoe Tara or Komba ~50 km N of Lomblen.... G. Indonesia: insights from crystal isotope stratigraphy. G. p.Emplacement of a debris avalanche during the 1883 eruption of Krakatau (Sunda Straits. Petrology 42. Gen. 2. Indonesia.pdf) (Lamongan volcan. 48. Res. Mineralogy and geochemistry indicate magma-crust interaction at Merapi more significant than previously thought. p. G. Sr isotopes in plagioclase compared to Wonosari Lst from Parangtritis) Charbonnier. S. 9. Provost & P. p.1 129 www. 123-128. (Internal archtecture of 2006 block-and-ash flow ) Charbonnier. 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