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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Suryono & M.C.G. Clarke (1982)- Primary tungsten occurrences in <strong>Sumatra</strong> and the <strong>Indonesia</strong>n tin islands. In:<br />
J.V. Hepworth (ed.) Tungsten <strong>Geology</strong> symposium, Jiangxi, China, 1981, ESCAP/RMRDC, p. 217-231.<br />
(In NE Bangka discontinuous serpentinites at Pemali Mine; viewed as trace <strong>of</strong> southern continuation <strong>of</strong> Triassic<br />
Raub-Bentong suture <strong>of</strong> Malay Peninsula by Pulunggono & Cameron 1984)<br />
Susanto, E., H. Priadi & P. Pathak (2008)- NSO Gas field simulation and production optimization. Proc. 32 nd<br />
Ann. Conv. Indon. Petrol. Assoc., IPA08-E-124, 18p.<br />
(Reservoir model <strong>of</strong> 1972 NSO gas discovery, 100km <strong>of</strong>f N <strong>Sumatra</strong>. Producing since 1999. 415' gas column in<br />
E-M Miocene Malacca Lst reefal buildup. Area ~7 x 10km, OGIP 2.7 TCF gas. NSO gas ~32.5% CO2 and<br />
1.5% H2S)<br />
Suseno, P.H., Zakaria, N. Mujahidin & E.A. Subroto (1992)- Contribution <strong>of</strong> Lahat Formation as hydrocarbon<br />
source rock in South Palembang Area, South Sumatera, <strong>Indonesia</strong>. Proc. 21st Ann. Conv. Indon. Petrol. Assoc.,<br />
1, p. 325-337.<br />
(Lahat or Lemat Fm mainly coarse volcanic rocks, but in some areas also claystone/ shale, like Benakat Shale.<br />
Such sediments organic-rich and in oil window. Mixed Type II- III kerogens may yield oil and gas. Biomarkers<br />
suggest Lahat and Talang Akar source rocks are identical)<br />
Susianto, A., E.S. Utoro & S. Grahia (2006)- Oligocene- Early Miocene paleogeography models South Balam<br />
Trough, Central <strong>Sumatra</strong> Basin. Proc. 35 th Ann. Conv. Indon. Assoc. Geol. (IAGI), Pekanbaru 2006,<br />
PITIAGI2006-053, 16p.<br />
(S Balam Trough one <strong>of</strong> most prolific petroleum systems in C <strong>Sumatra</strong> Basin. Paleogeographic maps made for<br />
three chronostratigraphic intervals. In Oligocene syn-rift time half grabens created with lake deposits in center<br />
(Pematang Brown Shale), bordered by fan deltas. Late Oligocene map <strong>of</strong> early post-rift phase illustrates<br />
Pematang Upper Red Bed formation deposition. In late post-rift Early Miocene more shallow marine influence,<br />
with fluvial and deltaic deposition (Menggala Fm))<br />
Susilawati, R. & C.R. Ward (2006)- Metamorphism <strong>of</strong> mineral matter in coal from the Bukit Asam deposit,<br />
South <strong>Sumatra</strong>, <strong>Indonesia</strong>. Int. J. Coal Geol. 68, p. 171-195.<br />
(Miocene coal <strong>of</strong> Bukit Asam in S <strong>Sumatra</strong> mostly sub-bituminous, consistent with regional burial. Effects <strong>of</strong><br />
Plio-Pleistocene igneous intrusions produced coal with vitrinite reflectance up to 4.17% (anthracite).<br />
Unmetamorphosed coals contain well-ordered kaolinite and quartz. Heat-affected coals, with Rv >1.0%,<br />
dominated by interstratified illite/smectite, poorly crystallized kaolinite and paragonite)<br />
Susilo, A., B.S. Widjiono & B. Setyanta (1999)- Gravity expression on the North end <strong>of</strong> the Bengkalis Trough.<br />
In: H. Darman & F.H. Sidi (eds.) Tectonics and Sedimentation <strong>of</strong> <strong>Indonesia</strong>, Indon. Sedim. Forum (FOSI),<br />
Spec. Publ. 1, p. 40-42.<br />
Susilohadi, S., C. Gaedicke & Y. Djajadihardja (2009)- Structures and sedimentary deposition in the <strong>Sunda</strong><br />
Strait, <strong>Indonesia</strong>. Tectonophysics 467, p. 55-71.<br />
(<strong>Sunda</strong> Strait opening initiated in early Late Miocene following M Miocene onset <strong>of</strong> <strong>Sumatra</strong> fault system.<br />
Three major graben systems/ pull-apart basins: W and E Semangko and Krakatau. Prior to Late Miocene most<br />
<strong>of</strong> <strong>Sunda</strong> Strait and surroundings probably developed in non-marine environment.)<br />
Susilohadi, S., C. Gaedicke & A. Ehrhardt (2005)- Neogene structures and sedimentation history along the<br />
<strong>Sunda</strong> forearc basins <strong>of</strong>f southwest <strong>Sumatra</strong> and southwest Java. Marine Geol. 219, 2-3, p. 133-154.<br />
(20 seismic lines in SW <strong>Sunda</strong> arc margin between Manna and W Java show fore-arc basin structures and<br />
stratigraphy since Late Paleogene. Paleomorphology <strong>of</strong> Cretaceous continental margin persisted until<br />
Oligocene and paleoshelf margin extended NW <strong>of</strong>f <strong>Sumatra</strong>. Two structural events between Late Oligocene-<br />
Pliocene. Back thrust-faulting along S border <strong>of</strong> fore-arc basin and initiation <strong>of</strong> Cimandiri FZ in Late<br />
Oligocene; <strong>Sumatra</strong> and Mentawai FZ initiated in Pliocene. Four Neogene sedimentary cycles. Volcanic<br />
activity abundant since late M Miocene. Turbidite deposition common along and seaward <strong>of</strong> basin slope during<br />
sea level lows in late M Miocene and L Miocene)<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 98 www.vangorselslist.com July 2012