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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Wisnu, A. & Nazirman (1997)- Statistic "direct HC indicator" terhadap keberadaan HC di blok Raja, Sumatera<br />
Selatan. Proc. 26th Ann. Conv. Indon. Assoc. Geol. (IAGI), Jakarta, Hidrokarbon, p. 71-88.<br />
Wissema, G.G. (1947)- Young Tertiary and Quaternary Gastropoda from the Island <strong>of</strong> Nias (Malay<br />
Archipelago). Doct. Thesis Univ. Leiden, p. 7-212.<br />
Wongsosantiko, A. (1976)- Lower Miocene Duri Formation sands, Central <strong>Sumatra</strong> Basin. Proc. 5th Ann.<br />
Conv. Indon. Petrol. Assoc., p. 63-76.<br />
(E Miocene Duri Fm sand reservoirs productive in 12 fields in C <strong>Sumatra</strong>. Deltaic sands, derived from North)<br />
Woodward, H. (1879)- Further notes on a collection <strong>of</strong> fossil shells, etc., from <strong>Sumatra</strong> (obtained by M.<br />
Verbeek, Director <strong>of</strong> the Geological Survey <strong>of</strong> the West Coast, <strong>Sumatra</strong>), Part III. Geol. Mag. 6, p. 492-500.<br />
Xie Chuanli, Ma Ha<strong>of</strong>an, Liang Honggang, Li Dongmei et al. (2007)- Alluvial fan facies and their distribution<br />
in the Lower Talang Akar Formation, Northeast Betara Oilfield, <strong>Indonesia</strong>. Petroleum Sci. 4, 2, p. 18-28.<br />
(Lower Talang Akar Fm in NE Betara Oilfield, Jabung Block, S <strong>Sumatra</strong>, in alluvial fan facies. Bed F coarse<br />
grained, poorly sorted and low quality. Conglomerates characterized by low gamma-ray, low resistance, high<br />
density and poor physical reservoir properties)<br />
Yabe, H. (1946)- On some fossils from the Saling Limestone <strong>of</strong> the Goemai Mts., Palembang, <strong>Sumatra</strong>- part 1.<br />
Proc. Japan Acad. 22, 6, p. 200-203. (online at http://www.journalarchive.jst.go.jp/… )<br />
(On 1943 examination in Bandung <strong>of</strong> thin sections <strong>of</strong> Saling Limestone in supposedly Cretaceous volcanic<br />
Saling Series <strong>of</strong> Gumai Mts. Presence <strong>of</strong> coral-like Lovcenipora and stromatoporoid Myriophorella. Saling<br />
limestone probably same age as U Jurassic Toriosu Lst <strong>of</strong> Japan. Saling series older than mid-Cretaceous<br />
Lingsing series quartz sst, shale with Orbitolina limestone. Relative age <strong>of</strong> formations is reverse <strong>of</strong> that<br />
suggested by Musper)<br />
Yabe, H. (1946)- On some fossils from the Saling Limestone <strong>of</strong> the Goemai Mts., Palembang, <strong>Sumatra</strong>- part 2.<br />
Proc. Japan Acad. 22, 8, p. 259-264.<br />
(L<strong>of</strong>tusia bemmeleni Silvestri from Saling Lst, S <strong>Sumatra</strong>, more likely Pseudocyclammina. Corals described<br />
from here not Lovcenipora but Late Jurassic Cladocoropsis miriabilis)<br />
Yancey, T.E. & S.A. Alif (1977)- Upper Mesozoic strata near Padang, West <strong>Sumatra</strong>. Bull. Geol. Soc. Malaysia<br />
8, p. 61-74.<br />
(U Jurassic- Lw Cretaceous Indarung Fm limestones and clastics exposed near Indarung, few km E <strong>of</strong> Padang.<br />
Carbonates wth coral-like Lovcenipora near base and bedded cherts (Ngalan Mb) near top. Indarung Fm used<br />
to determine ~200km <strong>of</strong> <strong>of</strong>fset along <strong>Sumatra</strong> fault zone. N.B.: Cherts subsequently dated as Aalenian, basal M<br />
Jurassic, by McCarthy et al. 2001; Lovcenipora believed to signify Late Triassic age by several authors; HvG)<br />
Yanto, Y. & T. Febriwan (2008)- AVO-inversion for reservoir characterization <strong>of</strong> Baturaja carbonate, Gunung<br />
Kembang Field, South <strong>Sumatra</strong> basin. Proc. 32 nd Ann. Conv. Indon. Petrol. Assoc., IPA08-G-047, 11p.<br />
(Gunung Kembang gas-oil field in E Miocene Baturaja Fm carbonates in anticlinorium with max. reservoir<br />
thickness 80m, gas cap 40 m, underlain by 8-12m oil column. AVO inversion used to map oil distribution.)<br />
Yarmanto & K. Aulia (1989)- Seismic expression <strong>of</strong> wrench tectonics in the Central <strong>Sumatra</strong> Basin.<br />
Geol.<strong>Indonesia</strong> (IAGI) 12, 1 (Katili Volume), p. 145-175.<br />
(Tertiary wrench faulting dominant in C <strong>Sumatra</strong> basin. Main deformation phases Pre-Tertiary, Eo-Oligocene<br />
and Plio-Pleistocene. Plio-Pleistocene deformation NW-SE, older structures trend mostly N-S)<br />
Yarmanto, T.L. Heidrick, Indrawardana & B.L. Strong (1995)- Tertiary tectonostratigraphic development <strong>of</strong> the<br />
Balam depocenter, Central <strong>Sumatra</strong> basin, <strong>Indonesia</strong>. Proc. 24 th Ann. Conv. Indon. Petrol. Assoc., p. 33-45.<br />
(Three major Tertiary tectonic- stratigraphic episodes in Balam Depocenter. Eocene (?)- Oligocene rifting (F1,<br />
±45–25.5 Ma) created N-NNW-trending half-grabens. Balam depocenter compartmentalized. Rift margin faults<br />
N-S (Manggala) or NNW-SSE (Jakun and Balam) and dip E-ENE at low-angles. ENE-trending Antara-Nella<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 120 www.vangorselslist.com July 2012