order feature parallels active subduction zone. Like present subduction zone, it is characterized by 2-3 fold increase in magnetic thickness in NE direction, probably reflecting past history <strong>of</strong> subduction in region) Purwaningsih, M.E.M., B. Mujihardi, L. Prasetya, W.A. Suseno & Y. Sutadiwirya (2006)- Structural evolution <strong>of</strong> the Jambi Sub-Basin: a rotated strike-slip mechanism. Proc. Jakarta 2006 Int. Geosc. Conf., Indon. Petrol. Assoc., Jakarta06-OT-60, 6p. (Extended Abstract) (Structural evolution <strong>of</strong> Jambi sub-basin three orders. Jambi sub-basin block rotation <strong>of</strong> 45° clockwise relative to Great <strong>Sumatra</strong> strike slip fault) Purwanti, Y., A. Bachtiar & A. Balfas (2003)- Petrophysics and organic geochemistry <strong>of</strong> basement section in Malacca Strait area. Proc. 32nd Ann. Conv. IAGI and 28th Ann. Conv. HAGI, Jakarta, 6p. (Basement in N-S trending Bengkalis Trough in Malacca Strait mainly meta-sediments and limestone in N, quartzite and mudstone in S. Hydrocarbon shows in some parts. TOC <strong>of</strong> basement shales from 0.11- 1.43%, Ro from 1.12- 4.33% (overmature). N area more mature than S. Tectonic uplift <strong>of</strong> block 2300' to 3850') Puspoputro, B. (1984)- Tinjauan atas hasil penyelidikan transiel di daerah kerja Pertamina. Proc. 12th Ann. Conv. Indon. Assoc. Geol. (IAGI), p. 127-134. (An overview <strong>of</strong> results <strong>of</strong> a transect study <strong>of</strong> Pertamina exploration block) Putra, D.D. (1999)- Analysis <strong>of</strong> the possible reserve in Eq. Baturaja Limestone by applying the bungin Batu geological model; a case study on the West <strong>of</strong> East Ketaling Structure, Jambi. Proc. 28th Ann. Conv. Indon. Assoc. Geol. (IAGI), 2, p. 99-114. Putrohari, R.D. (1992)- MSDC-1: a gas discovery in the Malacca Strait PSC, <strong>Sumatra</strong>, <strong>Indonesia</strong>. Proc. 21st Ann. Conv. Indon. Petrol. Assoc., p. 201-223. (MSDC-1 gas well on E margin <strong>of</strong> Bengkalis Trough, in pre-Sihapas objective. Structure Upper Oligocene inversion anticline. DC structure low relief hydrocarbon column exceeds mapped structural closure. Proposed geological model shows trapping mechanism partly stratigraphically controlled) Raguwanti, R., A. Sukotjo & B.W.H. Adibrata (2005)- Innovative approach using geostatistical inversion for carbonate reservoir characterization in Sopa Field, South <strong>Sumatra</strong>, <strong>Indonesia</strong>. Proc. 30 th Ann. Conv. Indon. Petrol. Assoc., 1, p. 61-66. (Geostatistical inversion <strong>of</strong> thin carbonate reservoir <strong>of</strong> Baturaja Fm in Sopa Field, South <strong>Sumatra</strong>) Rahmat, J. & S. Oemar (1998)- Exploration opportunities in the Bengkulu frontier basin, West <strong>Sumatra</strong>, <strong>of</strong>fshore <strong>Indonesia</strong>. In: J.L. Rau (ed.) Proc. 33 rd Sess. Co-ord. Comm. Coastal Offshore Geosc. Progr. E and SE Asia (CCOP), Shanghai 1996, 2, Techn. Reports, p. 114-127. (Hydrocarbon potential potential <strong>of</strong> Bengkulu fore-arc basin proven by presence <strong>of</strong> Oligocene or E Miocene brown shales with good TOC, onshore oil seeps and <strong>of</strong>fshore oil shows in wells. Potential reservoirs Baturaja and Parigi Fm equivalent carbonate buildups and E Miocene Talang Akar Fm equivalent sandstones. Temperature gradients in wells 2.8- 4.0 °C/ 100m) Rampino M.R. & S. Self (1992)- Volcanic winter and accelerated glaciation following the Toba super- eruption. Nature 359, 6390, p. 50-52. Rangin, C., X. Le Pichon & J. Lin (2007)- Docked or accreted Indian Ocean fracture ridges along the <strong>Sumatra</strong> subduction zone northern tip. AGU 2007 Fall Mtg., EOS Trans. Amer. Geoph. Un. 88, 52, Suppl, Abstract T31G-06 (Abstract only) Rashid, H., I.B. Sosrowidjojo & F.X. Widiarto (1998)- Musi Platform and Palembang High: a new look at the petroleum system. Proc. 26th Ann. Conv. Indon. Petrol. Assoc.,1, p. 265-276. (Musi Platform and Palembang High in S <strong>Sumatra</strong> important exploration targets. Source rocks Lahat/ Lemat Fm Paleogene lacustrine shales and fluvio-deltaic to marginal marine Talang Akar shales- coals. Three oil <strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 81 www.vangorselslist.com July 2012
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BIBLIOGRAPHY OF THE GEOLOGY OF INDO
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A widespread Plio-Pleistocene compr
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II.3. Natuna The Natuna area forms
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(Broad Oligo-Miocene paleogeographi
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Amin, T.C., Kusnama, E. Rustandi &
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(Pertamina operates 55 mature oil f
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(Heat flow in Central Sumatra basin
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Durham, J.W. (1940)- Triassic fossi
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