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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Lismawaty, K. Simanjuntak & A. Bachtiar (2010)- Studi provenance batupasir Formasi Sihapas daerah Gunung<br />
Tua- Sumatera Utara. Proc. 39th Ann. Conv. Indon. Assoc. Geol. (IAGI), Lombok, PIT-IAGI-2010-083, 15p.<br />
('Provenance study <strong>of</strong> Sihapas Fm sandstone, Gunung Tua area, North <strong>Sumatra</strong>')<br />
Liu, C.S., G.G. Shor & J.R. Curray (1991)- Velocity structure and nature <strong>of</strong> the forearc basin <strong>of</strong>f West <strong>Sumatra</strong><br />
from expanding spread experiments. Acta Oceanogr. Taiwanica 27, p. 21-39.<br />
Lohr, R. (1922) Beitrage zur Petrographie von Sud- <strong>Sumatra</strong> (West Palembang). Unpublished Dissertation<br />
Munster University, 65 p.<br />
('Contribution to the petrography <strong>of</strong> S <strong>Sumatra</strong> (W Palembang)'. Descriptions <strong>of</strong> rocks collected by H.M.E.<br />
Schurmann)<br />
Longley, I.M., R. Barraclough, M.A. Bridden & S. Brown (1990)- Pematang lacustrine petroleum source rocks<br />
from the Malacca Strait PSC, Central <strong>Sumatra</strong>, <strong>Indonesia</strong>. Proc. 19 th Ann. Conv. Indon. Petrol. Assoc., p. 279-<br />
299.<br />
(Wells on margins <strong>of</strong> Bengkalis Trough encountered Eocene-Oligocene Pematang Group lacustrine mudstones<br />
('Brown Shale') in shallow, immature sub-basin. Oil-source correlation suggests similar lacustrine sediments in<br />
Bengkalis Trough main source <strong>of</strong> oil in area. Relative 'deep' and 'shallow' lake and marginal lake sediments<br />
encountered, with characteristic palyno- and organo- facies. Anomalous low velocity and density <strong>of</strong> Brown<br />
Shale causes distinct seismic response, used to map extent <strong>of</strong> source)<br />
Longman, M.W., R.J. Maxwell, A.D.M. Mason & L.R. Beddoes (1987)- Characteristics <strong>of</strong> a Miocene intrabank<br />
channel in Batu Raja Limestone, Ramba field, South <strong>Sumatra</strong>, <strong>Indonesia</strong>. AAPG Bull. 71, p. 1261-1273.<br />
(Ramba Field produces from Lower Miocene reefal limestone buildup. Channel facies between buildups rel.<br />
tight and may act as lateral seal)<br />
Longman, M.W., C.T. Siemers & T. Siwindono (1992)- Characteristics <strong>of</strong> low-relief carbonate mudbank<br />
reservoir rocks, Baturaja Formation (Lower Miocene), Air Serdang and Mandala Fields, South <strong>Sumatra</strong> Basin,<br />
<strong>Indonesia</strong>. In: Carbonate rocks and reservoirs <strong>of</strong> <strong>Indonesia</strong>, a core workshop, Indon. Petrol. Assoc., p. 9.1 -9.11.<br />
(Air Serdang and Mandala fields reservoirs skeletal packstones in Lower Miocene Baturaja Fm at ~1500m.<br />
Reservoir rocks common fragments <strong>of</strong> branching corals with molluscs, and benthonic foraminifers in micritic<br />
and locally quite porous matrix, deposited in carbonate mudbanks draped over basement paleohigh during E<br />
Miocene marine transgression. Low-relief channels separate carbonate mudbanks)<br />
Lutz, R., K. Berglar, C. Gaedicke & D. Franke (2007)- Petroleum systems modelling in the Simeulue forearc<br />
basin <strong>of</strong>f <strong>Sumatra</strong>. AAPG Hedberg Conference, The Hague, p. (Abstract only)<br />
(Simeulue forearc basin <strong>of</strong>f N <strong>Sumatra</strong> explored by Union Oil from 1968-1978. Three wells encountered gas in<br />
carbonate reservoirs but none commercial. New 2D seismic by BGR (2006) shows 25 carbonate buildups, most<br />
in >1000 m water depth, showing backstepping geometry. Source rocks in area are not confirmed by drilling)<br />
Lutz, R., C. Gaedicke, K. Berglar, D. Franke, S. Schloemer & Y.S. Djajadihardja (2009)- Petroleum Systems <strong>of</strong><br />
the Simeulue Fore-arc Basin <strong>of</strong>f <strong>Sumatra</strong>, <strong>Indonesia</strong>. AAPG Int. Conf. Exhib., Rio de Janeiro, Brazil 2009,<br />
Expanded Abstract, 7 p.<br />
(online at: http://www.searchanddiscovery.net/documents/2010/10230lutz/ndx_lutz.pdf)<br />
(Short version <strong>of</strong> paper below)<br />
Lutz, R., C. Gaedicke, K. Berglar, S. Schloemer, D. Franke, & Y.S. Djajadihardja (2009)- Petroleum systems <strong>of</strong><br />
the Simeulue fore-arc basin, <strong>of</strong>fshore <strong>Sumatra</strong>, <strong>Indonesia</strong>. AAPG Bull. 95, 9, p. 1589-1616.<br />
(Fore-arc basins generally not considered as important petroleum provinces because <strong>of</strong> low heat flow.<br />
Simeulue fore-arc basin <strong>of</strong>f N <strong>Sumatra</strong> bright spots on seismic above potential carbonate platform reservoirs,<br />
with AVO/AVA analyses indicating presence <strong>of</strong> gas. Petroleum system modeling <strong>of</strong> assumed source rocks in<br />
Eocene and E-M Miocene reveals hydrocarbon generation is possible in main depocenters <strong>of</strong> C and S Simeulue<br />
Basin and may be more prolific than previously thought)<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 60 www.vangorselslist.com July 2012
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