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Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

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Santy, L.B. (2001)- Structural evolution <strong>of</strong> the North Bengkalis Trough, Malacca Straits, Central <strong>Sumatra</strong> Basin<br />

and its implication in creating traps for hydrocarbon accumulation. Proc. 28th Ann. Conv. Indon. Petrol. Assoc.,<br />

1, p. 739-747.<br />

(N Bengkalis Trough in Malacca Straits PSC. Exploration targets footwall traps <strong>of</strong> Padang Fault. Structural<br />

reconstruction shows four periods: (1) extension (Pematang time, Eocene -Oligocene?), creating N-S trending<br />

half graben in which Pematang Brown Shale source rock was deposited; (2) First compression (Menggala-<br />

Sihapas time, U Oligocene -E Miocene) NW- SE dextral strike-slip fault zone. Structural growth continued until<br />

Lower Sihapas time (3) Tectonic quiescence (Telisa time, E-M Miocene); (4) Second compression (M Miocene-<br />

Pliocene)<br />

Saputra, H.N. & B. Sapiie (2005)- Analogue study <strong>of</strong> basement fractured reservoirs in Kotopanjang Area,<br />

Central <strong>Sumatra</strong>. Proc. 30 th Ann. Conv. Indon. Petrol. Assoc., 1, p. 53- 60.<br />

Sardjito, E.F., Djumlati & S. Hansen (1991)- Hydrocarbon prospect <strong>of</strong> Pre Tertiary basement in Kuang Area,<br />

South <strong>Sumatra</strong>. Proc. 20th Ann. Conv. Indon. Petrol. Assoc., 1, p. 255-277.<br />

(Kuang area ~40 km S <strong>of</strong> Prabumulih, well known oil and gas producing area. Hydrocarbons structurally<br />

trapped in Baturaja and Talang Akar Fms. ASD-1 well proved hydrocarbons also in Pre-Tertiary fractured<br />

granodiorite and quartzite basement)<br />

Sarjono, S. & Sardjito (1989)- Hydrocarbon source rock identification in the South Palembang Sub-basin. Proc.<br />

18 th Ann. Conv. Indon. Petrol. Assoc., 1, p. 424-467.<br />

Sartono, S. & H. Murwanto (1990)- Kompleks melange di Sumatera Selatan, <strong>Indonesia</strong>. Proc 17th Ann. Conv.<br />

Indon. Assoc. Geol. (IAGI), Jakarta 1988 p. 65. (Abstract only?)<br />

('Melange complex in S <strong>Sumatra</strong>')<br />

Sartono, S. & R. Sinuraya (1985)- Kelompok Tapanuli di <strong>Sumatra</strong> Utara. Proc. 14th Ann. Conv. Indon. Assoc.<br />

Geol. (IAGI), p. 193-204.<br />

('The Tapanuli Group <strong>of</strong> North <strong>Sumatra</strong>')<br />

Sasajima, S, Y. Ot<strong>of</strong>uji, K. Hirook, S. Suparka & F. Hehuwat (1978)- Paleomagnetic studies on <strong>Sumatra</strong> Island:<br />

on the possibility <strong>of</strong> <strong>Sumatra</strong> being part <strong>of</strong> Gondwanaland. Rock Magnetism Paleogeoph. 5, p. 104-110.<br />

(Haile 1981: clockwise rotation <strong>of</strong> <strong>Sumatra</strong> since Triassic)<br />

Sato, K. (1991)- K-Ar ages <strong>of</strong> granitoids in Central <strong>Sumatra</strong>, <strong>Indonesia</strong>. Bull. Geol. Surv. Japan 42, p. 111-181.<br />

(online at: http://www.gsj.jp/Pub/Bull/vol_42/42-03_01.pdf)<br />

(K-Ar ages <strong>of</strong> 3 granitoid plutons in Barisan Mts, C <strong>Sumatra</strong>. Tourmaline-bearing biotite granite N <strong>of</strong> Sijunjung<br />

dated at 247 Ma,which may tie to Permian-Triassic tin granites <strong>of</strong> E Belt <strong>of</strong> Malay Peninsula.Two Late<br />

Cretaceous-Paleocene granodiorite-tonalites near <strong>Sumatra</strong>n Fault zone: Lassi pluton E <strong>of</strong> Solok (56 Ma) and<br />

Padangpanjang pluton S <strong>of</strong> Bukittinggi 64Ma. Petrography different from Late Cretaceous Hatapang pluton in<br />

N <strong>Sumatra</strong> (with tin-tungsten mineralization; 78-81 Ma age)<br />

Satrio, B. & Soejanto (1994)- Asih Field discovery: detailed structural reevalution along a wrench fault system<br />

in the Central <strong>Sumatra</strong> Basin, an exploration opportunity in a mature area. Proc. 23rd Ann. Conv. Indon. Assoc.<br />

Geol. (IAGI), 2, p. 1039-1049.<br />

Sayentika, Syafruddin & B. Sapiie (2003)- Eocene-Middle Miocene structural reconstruction <strong>of</strong> the Duri<br />

Anticline, Central <strong>Sumatra</strong> Basin, <strong>Indonesia</strong>. Proc 29th Ann. Conv. Indon. Petrol. Assoc. 1, p. 1-11.<br />

(At least four structural events in C <strong>Sumatra</strong> Basin: Pre-Tertiary basement development, Eocene-Oligocene<br />

rifting, M Miocene strike-slip and M Miocene-Recent compression. Duri Anticline reconstruction using<br />

flattened seismic lines)<br />

<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 87 www.vangorselslist.com July 2012

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