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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Guntoro, A. & Y.S. Djajadiharja (2005)- Tectonic scenario <strong>of</strong> the <strong>Sumatra</strong> fore-arc basin in relation to the<br />
formation <strong>of</strong> petroleum systems. In: Int. Conf. <strong>Geology</strong>, Geotechnology and Mineral Resources <strong>of</strong> Indochina<br />
(GEOINDO 2005), Khon Kaen, Thailand, p.<br />
Guntur, A., S. Hastuti, B. Situmorang & B. Yulihanto (1993)- Studi fasies dan batuan asal formasi<br />
Sawahtambang cekungan Ombilin, <strong>Sumatra</strong> Barat. Proc. 22nd Ann. Conv. Indon. Assoc. Geol. (IAGI) 2, p.<br />
1028-1043.<br />
(‘Study <strong>of</strong> rocks and facies <strong>of</strong> Sawahtambang Fm, Ombilin Basin, W <strong>Sumatra</strong>’)<br />
Guntur, A., R.S. Himawan & B. Situmorang (1992)- The formation and evolution <strong>of</strong> Paleogene Talawi Graben,<br />
Ombilin Basin, West <strong>Sumatra</strong>. Proc. 21st Ann. Conv. Indon. Assoc. Geol. (IAGI), 2, p. 565-584.<br />
Gutomo, A. & M.B. Satyawan (1995)- Development concept <strong>of</strong> Rantau Field based on 3-D seismic data. Proc.<br />
24th Ann. Conv. Indon. Petrol. Assoc., 2, p. 583-<br />
Guttormsen, J. (2010)- Naturally fractured basement reservoirs: using South <strong>Sumatra</strong> to characterize the<br />
challenges <strong>of</strong> exploring and exploiting fracture basement reservoirs. Proc. 34th Ann. Conv. Indon. Petrol.<br />
Assoc., IPA10-G-183, 15p.<br />
(Data from S <strong>Sumatra</strong> fracture basement reservoirs <strong>of</strong> Suban, Sumpal, and Dayung gas fields. Fractured<br />
reservois include granite, Permian meta-limestone (Leko), quartzites and pelitic rocks (phyllites and schists). In<br />
S <strong>Sumatra</strong> metasediments dominant reservoir lithology, but better test rates in granites and meta-carbonates)<br />
Guttormsen, J., R. Achiat, R. Indrawan & R. Waworuntu (2009)- Phyllitic fractured reservoirs <strong>of</strong> Southern<br />
<strong>Sumatra</strong>. Proc. 33 rd Ann. Conv. Indon. Petrol. Assoc., IPA09-G-149, p. 257-272.<br />
(Major accumulations <strong>of</strong> hydrocarbons in fractured metasedimentary reservoirs in S <strong>Sumatra</strong> Basin. Basement<br />
composed <strong>of</strong> Permian- Cretaceous sediments, intruded by felsic magmas)<br />
Gutzwiller, E. (1914)- Petrografische beschrijving der eruptiefgesteenten van het Goemai-gebergte. Jaarboek<br />
Mijnwezen Nederl. Oost-Indie 41 (1912), Verhand., p. 50-86.<br />
(Petrographic descriptions <strong>of</strong> igneous rocks from Gumai Mountains, collected by Tobler: Pre-Tertiary granites,<br />
porphyrites, diabase, tuffs and Young Tertiary liparite, dacite, andesite, basalt)<br />
Haanstra, U. & E. Spiker (1932)- Uber jungneogene Molluskenfaunen aus den Residenzen Benkoelen und<br />
Palembang, S.W. <strong>Sumatra</strong>. Proc. Kon. Nederl. Akad. Wetensch., Amsterdam, 35, 10, p. 1313-1324.<br />
(Online at: http://www.dwc.knaw.nl/DL/publications/PU00016359.pdf)<br />
(‘On Late Neogene mollusk faunas from the Bengkulu and Palembang Residencies, SW <strong>Sumatra</strong>’. Molluscs<br />
from Bengkulu area collected by Erb in 1902 along coast between Bengkulu and Krue (72 species, 36% Recent,<br />
suggesting Late Neogene age), and from Lower Palembang Fm at Talang Akar anticline N <strong>of</strong> Talang Abab,<br />
Palembang Province (50 species, 26% Recent, suggesting Miocene age))<br />
Hadi, T. & B. Simbolon (1976)- The carbonate rocks <strong>of</strong> the Batu Raja Formation in its type locality, Batu Raja,<br />
South <strong>Sumatra</strong>. Proc. Carbonate Seminar, Jakarta 1976, Indon. Petrol. Assoc., Spec. Vol., p. 67-78.<br />
(Baturaja Fm in Baturaja area <strong>of</strong> S <strong>Sumatra</strong> bedded limestones in lower, massive limestones in upper part.<br />
Texture <strong>of</strong> limestones varies from reef (boundstone) to wackestone and wacke-packstone and suggest<br />
depositional environments from open shoal reef, fore reef, transition to open basin to open littoral back reef)<br />
Hadiyanto (1992)- Organic petrology and geochemistry <strong>of</strong> the Tertiary formations at Meulaboh area, West<br />
Aceh Basin, Sumatera, <strong>Indonesia</strong>. Ph.D. Thesis, University <strong>of</strong> Wollongong, Australia, p. 1-219.<br />
(online at: http://ro.uow.edu.au/theses/1397/) (Meulaboh forearc basin with thick succession <strong>of</strong> Oligocene-<br />
Pliocene coal-bearing sediments. Coal and clastic rocks potential source rocks but mostly immature and have<br />
not produced significant liquid hydrocarbons. Late Oligocene- E Miocene Tangla Fm shales and M Miocene<br />
Kueh Fm best source rocks. Oligocene coal and possibly Miocene coal good hydrocarbon generation potential.<br />
Onshore vitrinite reflectance gradients greater than <strong>of</strong>fshore, so oil window predicted to be shallower onshore)<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 36 www.vangorselslist.com July 2012