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Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

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Terpstra, H. (1932)- The joint systems in the vicinity <strong>of</strong> the Salida Mine (West coast <strong>of</strong> <strong>Sumatra</strong>). Proc. Kon.<br />

Nederl. Akad. Wetensch., Amsterdam, 35, p. 891-897.<br />

(online at: http://www.dwc.knaw.nl/DL/publications/PU00016298.pdf)<br />

(Four groups <strong>of</strong> orientation <strong>of</strong> quartz veins in Salida mine area: N30°E, N40°W, N10°E, N90°E)<br />

Terres, R.R. & Soejanto (1995)- Central <strong>Sumatra</strong> prospect evaluation, structural and stratigraphic fluid barriers<br />

and hydrodynamic systems as indicated by wireline formation pressures. Proc. 24th Ann. Conv. Indon. Petrol.<br />

Assoc., 1, p. 19-32.<br />

Tesch, P. (1916)- Permische trilobieten van Atjeh. Tijdschr. Kon. Ned. Aardrijksk. Gen. Ser. 2, 33, p. 610-611.<br />

('Permian trilobites from Aceh'. Two species <strong>of</strong> trilobite casts in dark red, tuffaceous marly rock, associated<br />

with corals, crinoids, brachiopods and gastropods, previously reported by Klein 1916 as presumably Devonian.<br />

Species very similar those described form Permian in Timor)<br />

Thamrin, H.M. (1985)- Studi pendahuluan prospek batubara di lapangan Benuang <strong>Sumatra</strong> Selatan. Proc. 14th<br />

Ann. Conv. Indon. Assoc. Geol. (IAGI), p. 223-231.<br />

('Preliminary study <strong>of</strong> coal prospects in the Benuang field, S <strong>Sumatra</strong>')<br />

Thamrin, M. (1980)- Heat-flow in the Tertiary basin <strong>of</strong> North <strong>Sumatra</strong>, <strong>Indonesia</strong>. Proc. 17th Sess. Comm. Coord.<br />

Joint Prosp. Min. Res. in Asian Offshore Areas (CCOP), Bangkok, p. 394-408.<br />

Thamrin, M., Siswoyo, S. Sandjojo, Prayitno & S. Indra (1980)- Heat flow in the Tertiary basin <strong>of</strong> South<br />

<strong>Sumatra</strong>, <strong>Indonesia</strong>. Proc. 16th Sess. Comm. Co-ord. Joint Prosp. Min. Res. in Asian Offshore Areas (CCOP),<br />

Bandung 1979, p. 250-271.<br />

(Heat flow <strong>of</strong> S <strong>Sumatra</strong> basin determined from 358 wells in 54 oil fields. Average heatflow 2.58 Mcal/cm sec.<br />

Centre <strong>of</strong> basin rel. cool with 3 HFU)<br />

Thesly, H.D., D.S. Asra, E.I. Gartika, T. Febriwan & J.J.Wood (2010)- Integrated geology and reservoir study<br />

in determining hydrocarbon reserves in Pangkal field, South <strong>Sumatra</strong>. Proc. 39th Conv. Indon. Assoc. Geol.<br />

(IAGI), Lombok, PIT-IAGI-2010-170, 8p.<br />

(Reserves study <strong>of</strong> Pangkal field in Palembang High area, S <strong>Sumatra</strong> basin, NE <strong>of</strong> Kaji Semoga field (= Medco<br />

Langkap field). Discovered in 1987; 35 wells drilled; current production 1400 BOPD from 14 wells. Reservoir<br />

Talang Akar Fm stacked fluvial channel sandstones with 15-21% porosity. OOIP <strong>of</strong> field is 24 MMBO, EUR 7<br />

MMBO, cumulative oil production 5 MMBO)<br />

'T Hoen, C.W.A. (1922)- Verslag over het onderzoek der Tertiaire petroleumterreinen ter Oostkust van Atjeh<br />

(terrein Atjeh II). Jaarboek Mijnwezen Nederl. Indie 48 (1919), Verhand. 1, p. 163-229.<br />

('Investigation <strong>of</strong> the Tertiary petroleum terrains <strong>of</strong> the East coast <strong>of</strong> Aceh (terrain Aceh II), N <strong>Sumatra</strong>')<br />

'T Hoen, C.W.A. (1931)- Mededeeling over een vondst van diamanten in de Siaboe Rivier, ten zuiden van<br />

Bangkinang (Midden-<strong>Sumatra</strong>). De Mijningenieur 13, p. 176-178.<br />

('Communication on a discovery <strong>of</strong> diamonds in the Siabu River, S <strong>of</strong> Bangkinang (C <strong>Sumatra</strong>)'. About 150<br />

small diamonds found during exploration for tin ore. Bedrocks is Tertiary clay-shales and granite. Diamonds<br />

were found in the parts <strong>of</strong> the kaksa richest in tin ore)<br />

'T Hoen, C.W.A. (1932)- Oliesporen in het Oembilin kolenveld. De Mijningenieur 13, p. 194<br />

('Oil traces in the Ombilin coal field'. Exploration well penetrated coal between 190-208m and another thin<br />

(20cm) coal at 272m. At 283m a 4m thick oil-stained sandstone from which a few liters <strong>of</strong> oil were obtained)<br />

Thomas, L.P. (2005)- Fuel resources: coals. In: A.J. Barber, M.J. Crow & J.S. Milsom (eds.) <strong>Sumatra</strong>- geology,<br />

resources and tectonic evolution, Geol. Soc., London, Mem. 31, p. 142-146.<br />

(Brief overview <strong>of</strong> coal distribution in N, C and S <strong>Sumatra</strong>. Producing mines only in Central <strong>Sumatra</strong> (Ombilin;<br />

Eocene-Oligocene), S <strong>Sumatra</strong> (Late Miocene- Pliocene) and Bengkulu (Miocene) Basins)<br />

<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 103 www.vangorselslist.com July 2012

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