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Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

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(Radiometric age dates from <strong>Sumatra</strong>, Java, <strong>Natuna</strong>, etc.)<br />

Katili, J.A. (1974)- <strong>Sumatra</strong>. In: A.M.Spencer (ed.) Mesozoic-Cenozoic Orogenic Belts, Geol. Soc. London,<br />

Spec. Publ. 4, p. 317-331.<br />

Katili, J.A. & F. Hehuwat (1967)- On the occurrence <strong>of</strong> large transcurrent faults in <strong>Sumatra</strong>, <strong>Indonesia</strong>. J.<br />

Geosci. Osaka City Univ. 10, 1, p. 5-17.<br />

(Several geologic features suggesting 20-25km right-lateral slip along <strong>Sumatra</strong> fault zone)<br />

Katili, J.A. & Kamal (1961)- Laporan sementara mengenai geologi daerah Ombilin Pesisir utara Danau<br />

Singkarak. Proc. Inst. Tekn. Bandung 1, 1, p. 5-23.<br />

(online at: http://journal.itb.ac.id/index.php?li=article_detail&id=836)<br />

(Geological mapping in Ombilin area N <strong>of</strong> Lake Singkarak to study Late Paleozoic- E Mesozoic Silungkang<br />

Fm volcanic-sedimentary deposits, Triassic and 'Pre-Permian' Guguk Bulat granite. Fusulinids <strong>of</strong> Silungkang<br />

Fm determined as Permian by P. Marks. Part <strong>of</strong> limestone in Lurah Tambang River not Triassic, but<br />

Silungkang Fm. Pre-Permian granite does not exist; arkosic rock <strong>of</strong> Guguk Bulat part <strong>of</strong> Tertiary quartz<br />

sandstone formation, resulting from weathering <strong>of</strong> granite <strong>of</strong> possible Cretaceous age)<br />

Kato, M., D. <strong>Sunda</strong>ri, T.C. Amin, D. Kosasih, S.L. Tobing et al. (1999)- A note on the reconfirmation <strong>of</strong> Lower<br />

Carboniferous age <strong>of</strong> the Agam River limestone <strong>of</strong> the Kuantan Formation, West <strong>Sumatra</strong>. Geol. Res. Dev.<br />

Centre, Bandung, Paleont. Ser. 9, p. 53-61.<br />

(Corals in Agam River limestone in Padang Highlands E <strong>of</strong> Bukittingi confirm E Carboniferous, Visean age)<br />

Katz, B.J. & W.C. Dawson, (1997)- Pematang-Sihapas petroleum system <strong>of</strong> Central <strong>Sumatra</strong>.. In: J.V.C. Howes<br />

& R.A. Noble (eds.) Proc. Conf. Petroleum Systems <strong>of</strong> SE Asia and Australasia, Indon. Petrol. Assoc., p. 685-<br />

698.<br />

(Lacustrine Pematang Group Brown Shale Fm generated -60 GB oil. E Miocene Sihapas sandstones principal<br />

reservoirs. Giant fields (Minas, Duri) principally along E margins <strong>of</strong> sub-basins. Smaller fields with Pematang<br />

nonmarine reservoirs in deeper troughs. Pematang Group in series <strong>of</strong> grabens, with basal fluvial/alluvial unit<br />

(Lower Red Bed), medial lacustrine unit (Brown Shale), upper fluvial/alluvial unit (Upper Red Bed). Pematang<br />

disconformably overlain by Menggala Fm with quartzose- subarkosic sandstones with average porosity >20%<br />

and permeability <strong>of</strong> 1500 md. Many oil fields associated with paleohighs, drag folds, and post mid-Miocene<br />

inversion. Hydrocarbon generation initiated in Miocene and continues currently in parts <strong>of</strong> basin)<br />

Katz, B.J., W.C. Dawson, C. Atallah, B. Gunardi et al. (1998)- Anatomy <strong>of</strong> a lacustrine source- the Brown<br />

Shale <strong>of</strong> Central <strong>Sumatra</strong>, <strong>Indonesia</strong>. AAPG Ann. Mtg., Salt Lake City 1998 (Abstract)<br />

(Brown Shale Fm <strong>of</strong> Pematang Group lacustrine source rock, with oil-prone facies in more rapidly subsiding<br />

sub-basins and more distal settings. Oil-prone facies in upper portion <strong>of</strong> sequence. Multiple oil sub-families,<br />

reflecting environmental variations (water depth, salinity, etc.) and relative proportion <strong>of</strong> allochthonous<br />

organic matter. Oil sub-families geographically restricted, and associated with distinct sub-basin)<br />

Katz, B.J. & B. Mertani (1989)- Central <strong>Sumatra</strong>- a geochemical paradox. Proc. 18th Ann. Conv. Indon. Petrol.<br />

Assoc., p. 403-425.<br />

Kavalieris, I., D.J. Turvey & L.J.L. Heesterman (1987)- The geology and mineralization <strong>of</strong> the Mangani Mine,<br />

<strong>Sumatra</strong>, <strong>Indonesia</strong>. In: E. Brennan (ed.) Proc. Pacific Rim Congress 1987, Gold Coast, Australasian Inst.<br />

Mining Metallurgy, Parkville, p. 221-225.<br />

(Historically important but small Mangani gold-silver mine was discovered in 1907, exploited between 1912-<br />

1931 and 1940-1941. Located along splay <strong>of</strong> NW-SE trending <strong>Sumatra</strong>n Fault System. Mineralization young<br />

low sulfur type epithermal system, hosted by Tertiary andesite)<br />

Keats, W. (1981)- Cainozoic sedimentation in <strong>Sumatra</strong> north <strong>of</strong> 3°N. In: Proc. Second Symp. Integrated<br />

geological survey <strong>of</strong> northern <strong>Sumatra</strong>. Laporan Simposium Direktorat Sumber Daya Mineral, Direct. Min.<br />

Res., Bandung, 3A, p. 87-101.<br />

<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 52 www.vangorselslist.com July 2012

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