Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
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(Heat flow in Central <strong>Sumatra</strong> basin <strong>of</strong> calculated from 92 wells. Average gradient 3.7 °F/ 100 ft (67.6°C/km)<br />
and average heat flow <strong>of</strong> 3.27 ± 0.93 HFU, twice world average. Gradient and heat flow vary inversely with<br />
depth. Heat flow in N <strong>Sumatra</strong> basin, S <strong>Sumatra</strong> Basin, <strong>Sunda</strong> Strait and W Java is 2.5 HFU, while in Java E <strong>of</strong><br />
110°E it drops to 1.9 HFU)<br />
Daulay, B. & H. Nursarya (1996)- Petrografi batubara: aplikasinya terhadap lingkungan pengendapan di daerah<br />
Bengkulu. Proc. 25th Ann. Conv. Indon. Assoc. Geol. (IAGI), 2, p. 531-541.<br />
('Coal petrography: its application towards depositional environments in the Bengkulu area')<br />
Daulay, B. & B. Santoso (2008)- Characteristics <strong>of</strong> selected Sumateran Tertiary coals regarding their<br />
petrographic analysis. Indon. Mining J. 11, 10, p. 1-18.<br />
(Type and rank variation <strong>of</strong> Ombilin and Bukit Asam Tertiary coals assessed in 170 samples. Coals dominated<br />
by vitrinite, common liptinite and rare inertinite and mineral matter. Higher vitrinite reflectance <strong>of</strong> some coals<br />
result <strong>of</strong> the local igneous intrusions in both areas)<br />
Davies, P.R. (1984)- Tertiary structural evolution and related hydrocarbon occurrences, North <strong>Sumatra</strong> Basin.<br />
Proc. 13 th Ann. Conv. Indon. Petrol. Assoc., p. 19-49.<br />
(N <strong>Sumatra</strong> along trailing edge <strong>of</strong> counterclockwise (CCW) rotating '<strong>Sunda</strong> Microplate' in Tertiary. Eocene-<br />
Lower Oligocene high-angle convergence between <strong>Sunda</strong> and Indian-Australian Plates generated Npropagating,<br />
dextral, overstepping wrench faults along W edge <strong>of</strong> microplate. Late Oligocene CCW rotation <strong>of</strong><br />
<strong>Sunda</strong> Microplate result <strong>of</strong> rifting in Thai and Malay basins. N <strong>Sumatra</strong> basin developed in Late Oligocene- E<br />
Miocene as horst and graben structures between reactivated dextral wrench faults along W edge <strong>of</strong> microplate.<br />
E-M Miocene uplift reactivated earlier rifted structures <strong>of</strong> N <strong>Sumatra</strong> basin, causing widespread erosion,<br />
followed by subsidence and first marine deposits. Second phase <strong>of</strong> <strong>Sunda</strong> CCW rotation in late M Miocene,<br />
continuing to present day, caused by emplacement <strong>of</strong> oceanic crust in Andaman Sea. Renewed convergence<br />
since late M Miocene at less acute angle, causing compression, inception <strong>of</strong> subduction complex along W edge<br />
<strong>Sumatra</strong>, uplift <strong>of</strong> Barisan Mountains, and regressive sedimentation across N <strong>Sumatra</strong> basin. Evolution <strong>of</strong> N, C<br />
and S <strong>Sumatra</strong>n basins essentially identical)<br />
Davies, P.R. (1989)- Tectonics <strong>of</strong> North <strong>Sumatra</strong>. In: B. Situmorang (ed.) Proc. 6th Reg. Conf.<strong>Geology</strong> Mineral<br />
Hydrocarbon Res. Southeast Asia, Jakarta 1987, Indon. Assoc. Geol. (IAGI), p. 207-227.<br />
(Tertiary structural evolution <strong>of</strong> N <strong>Sumatra</strong> described as consequence <strong>of</strong> its position along trailing edge <strong>of</strong><br />
counterclockwise rotating <strong>Sunda</strong> microplate, starting in Late Oligocene.)<br />
Davis, R.C., W.O. Ardjakusumah & I.S. Soemantri (1998)- Kinetic modeling <strong>of</strong> the Pematang-Sihapas(!)<br />
petroleum system, Malacca Strait PSC, Central <strong>Sumatra</strong>. Proc. 26th Ann. Conv. Indon. Petrol. Assoc. 1, p. 35-<br />
50.<br />
(Principal and probably only source rock for Malacca PSC oil is Paleogene Pematang Group lacustrine Brown<br />
Shale Mb., mature in Bengkalis Graben. Modeling indicates discovery farthest from Bengkalis kitchen likely<br />
sourced by long distance migration (~25 km), as local sub-basin (Rangsang Trough) is immature. Other subbasin<br />
(Padang Trough) highly mature due to very high geothermal gradient. Heating event responsible for<br />
petroleum expulsion extremely recent in C <strong>Sumatra</strong> Basin)<br />
Dawson, W.C. & T.H. Tankersley (1997)- Incised valley sandstone reservoirs: Kotabatak Field, Central<br />
<strong>Sumatra</strong> basin, <strong>Indonesia</strong>- case example. In: K.W. Shanley & B.F. Perkins (eds.) Shallow marine and nonmarine<br />
reservoirs, Gulf Coast Sect. SEPM, 18 th Ann. Res. Conf., Houston 1997, p. 81-91.<br />
De Beaufort, L.F. (1925)- Het voorkomen van een osteoglosside visch in het Tertiair van <strong>Sumatra</strong>. Verhand.<br />
Geol. Mijnbouwk. Gen. Nederl. Kol., Geol. Ser. 8 (Verbeek volume), p. 49-52.<br />
('The occurrence <strong>of</strong> an osteoglossid fish in the Tertiary <strong>of</strong> <strong>Sumatra</strong>'. Discussion <strong>of</strong> Eocene fresh water bone-<br />
fish in C <strong>Sumatra</strong>, collected by Verbeek and Tobler. Described in more detail by Sanders 1934)<br />
De Bruijn Kops, G.F. (1853)- Tocht naar de Reteh Rivier ter onderzoeking van steenkolenlagen. Natuurk.<br />
Tijdschr. Nederl. Indie 4, p. 611-626.<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 24 www.vangorselslist.com July 2012
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