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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Kingston, J. (1978)- Oil and gas generation, migration and accumulation in the North <strong>Sumatra</strong> Basin. SEAPEX<br />
Proc. 4, Singapore 1977/78, p. 158-182.<br />
(N <strong>Sumatra</strong> Tertiary source rocks are deep in basin and older than lower Middle Miocene)<br />
Kirby, G.A., R.J. Morley, B. Humphreys, C.J. Matchette-Downes, M.J. Sarginson, G.K. Lott et al. (1993)- A reevaluation<br />
<strong>of</strong> the regional geology and hydrocarbon prospectivity <strong>of</strong> the onshore central North <strong>Sumatra</strong> basin.<br />
Proc. 21 st Ann. Conv. Indon. Petrol. Assoc., 1, p. 243-264.<br />
(BGS/ LEMIGAS study <strong>of</strong> onshore central N <strong>Sumatra</strong> Basin. Results indicate possibility <strong>of</strong> hydrocarbons in<br />
stratigraphic traps and closures in Miocene sediments and Palaeogene half-grabens which are believed to have<br />
been source kitchens. Marine mudstones poor source potential for gas only. Source rocks probably lacustrine,<br />
very mature, located in Palaeogene half grabens. Oil generation began at ~11 Ma in deepest <strong>of</strong> half-grabens)<br />
Kirby, G.A., B. Situmorang & B. Setiardja (1989)- Seismic stratigraphy <strong>of</strong> the Baong and Keutapang<br />
Formations, North <strong>Sumatra</strong> Basin. Proc. 18th Ann. Conv. Indon. Petrol. Assoc. 1, p. 289-301.<br />
(Seismic stratigraphy <strong>of</strong> M-L Miocene sandstones in Pertamina Unit I area, N <strong>Sumatra</strong>. Dominantly deltaic<br />
sequences <strong>of</strong> Keutapang Fm in S and the marine Upper Baong Shale to N. Three separate phases <strong>of</strong> delta<br />
progradation. Clastic source directions mainly from SSW and SW, from rising Barisan Mountains. Besitang<br />
River Sst in NE from continental source in East)<br />
Kjellgren, G.M. & H. Sugiharto (1989)- Oil geochemistry: a clue to the hydrocarbon history and prospectivity<br />
<strong>of</strong> the southeastern North <strong>Sumatra</strong> Basin, <strong>Indonesia</strong>. Proc. 18th Ann. Conv. Indon. Petrol. Assoc., p. 363-384.<br />
(Oils from onshore and <strong>of</strong>fshore N <strong>Sumatra</strong> basin two separate phases. Oldest severely biodegraded and<br />
probably expelled from syn-rift E Oligocene Bampo Fm. Widespread post-rift Late Oligocene- M Miocene<br />
Lower Baong/Belumai Fm is source for second and final oil phase)<br />
Klein, W.C. (1916)- On a trilobite fauna <strong>of</strong> presumably Devonian age in the Dutch East Indies near Kaloee,<br />
Tamiang District, S.E. Atjeh). Proc. Kon. Nederl. Akad. Wetensch., Amsterdam, 18, 2, p. 1632-1636.<br />
(online at: http://www.dwc.knaw.nl/DL/publications/PU00012632.pdf)<br />
(Discovery <strong>of</strong> presumably Devonian limestones with trilobites W <strong>of</strong> Kaloee on Simpang Kiri River, SE Aceh, in<br />
190m thick, weakly folded limestone-shale succession. Trilobite probably <strong>of</strong> genus Proetus. Associated with<br />
brachiopods, corals and crinoids. No map or illustrations. Trilobite subsequently determined to be Permian in<br />
age by Tesch, 1916)<br />
Klein, W.C. (1918)- De Oostoever van het Toba-meer in Noord-<strong>Sumatra</strong>. Jaarboek Mijnwezen Nederl. Oost-<br />
Indie 46 (1917), Verh. 1, p. 136-187.<br />
(Geologic description <strong>of</strong> eastern shore <strong>of</strong> Lake Toba, N <strong>Sumatra</strong>, with 1:200,000 geologic map)<br />
Klein, W.C. (1918)- Voorloopige mededeeling over de geologie van den oostoever van het Tobameer in N.-<br />
<strong>Sumatra</strong>. Natuurk. Tijdschr. Nederl.-Indie 77, 3, p. 206-216.<br />
(‘Preliminary communication on the geology <strong>of</strong> the eastern shore <strong>of</strong> Lake Toba, N <strong>Sumatra</strong>’. Two amphibolebiotite<br />
granite massifs intruded into highly folded Paleozoic limestones and slates, overlain by little- folded<br />
?Eocene quartz sandstones, liparite tuffs and andesite intrusives. Old lake terraces up to 250m above present<br />
lake level)<br />
Klompe, Th.H.F. (1954)- On the supposed Upper Paleozoic unconformity in North <strong>Sumatra</strong>. Madjalah Ilmu<br />
Alam untuk <strong>Indonesia</strong> (Indon. J. Nat. Sci.) 111, p. 151-165. (also 1955 Leidsche Geol. Meded. 20, p. 120-134)<br />
(No obvious Paleozoic- Mesozoic unconformity along NE shore lake Toba, but folded Upper Triassic shales-<br />
limestones unconformably overlain by Tertiary clastics (Paleogene conglomerates, E Miocene marine shale)<br />
Knight, M.D., G.L. Walker, B.B. Ellwood & J.F. Diehl (1986)- Stratigraphy, palaeomagnetism, and magnetic<br />
fabric <strong>of</strong> the Toba tuffs: constraints on sources and eruptive styles. J. Geoph. Res. 91, p. 355-382.<br />
Kobayashi, T. & K. Masatani (1968)- Upper Triassic Halobia (Pelecypoda) from North <strong>Sumatra</strong> with a note on<br />
the Halobia facies in <strong>Indonesia</strong>. J. Geol. Geogr. Japan, 39, 2-4, p. 113-123.<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 54 www.vangorselslist.com July 2012