Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

deltaic regressive sequence. Erosion of Barisan Mountains generated Plio-Pleistocene deltaic/slope deposits
which prograde onto E flank of Sumatran forearc basin)
Huchon, P. & X. Le Pichon (1984)- Sunda Strait and central Sumatra fault. Geology 12, p. 668- 672.
(Right-lateral Central Sumatra fault accommodates oblique subduction and terminates in SE at extensional
zone of Sunda Strait)
Hudya, F.D., A. Aimar, T. Afandi, D. Setiawan & R.S.W. Handayani (2008)- Recovery optimization strategy
for thin oil column reservoir with large gas cap: case study of Gunung Kembang Field. Proc. SPE Asia Pacific
Oil & Gas Conf., Perth 2008, 7 p.
(Exploitation of thin (25’-40’) oil rim below thick gas cap in Gunung Kembang field challenging. Horizontal oil
wells in upper oil rim near gas oil contact best strategy for depletion of oil rim. Oil recovery expected to rise to
~ 8% while gas is being delivered)
Humphreys B., et. al. (1994)- Origin of grain-coating chlorite by smectite transformation: an example from
Miocene sandstones, North Sumatra back-arc basin, Indonesia. Clay Minerals 29, 4, p. 681-692.
Hutapea, O.M. (1976)- Depositional environments and their control of oil accumulation in the Abab field, South
Sumatra. J. Assoc. Indon. Geol. (IAGI) 3, 1, p. 37-43.
Hutapea, O.M. (1978)- Pengembangan lapangan Benakat: suatu perangkap stratigrafi. Geol. Indon. (J. Indon.
Assoc. Geol., IAGI) 5, 1, p. 45-57.
('Development of the Benakat field; some stratigraphic traps'. S Sumatra)
Hutapea, O.M. (1981)- Pewatasan lapisan waduk Formasi Tualang, di Merbau, Riau. Proc. 10th Ann. Conv.
Indon. Assoc. Geol. (IAGI), p. 222-229.
('Traps in the Tualang Fm at Merbau, Riau')
Hutapea, O.M. (1981)- The prolific Talang Akar Formation in Raja Field South Sumatra. Proc. 10 th Ann. Conv.
Indon. Petrol. Assoc., p. 251-267.
(S Sumatra Raja field 1940 discovery in Late Oligocene- E Miocene deltaic- shallow marine Talang Akar Sst)
Hutapea, O. (1998)- The Semoga- Kaji discoveries: large stratigraphic Batu Raja oil fields in South Sumatra.
Proc. 26th Ann. Conv. Indon. Petrol. Assoc., 1, p. 313-326.
(Semoga, Kaji and Sembada first E Miocene Baturaja carbonates discoveries on Palembang High and with
stratigraphic trapping components. In Rimau Block only Talang Akar Fm had been productive. Good quality
reef-related carbonate reservoir. Hydrocarbons from Talang Akar and Lemat Fm lacustrine shales, trapped by
combination structural- stratigraphic controls, after initial migration into paleo-traps, then remigrating into
present traps. Telisa shales acts as top seal, facies change of Baturaja carbonates acts as lateral seal)
Hutapea, O. (2002)- What makes Kaji-Semoga field so big? In: F.H. Sidi & A. Setiawan (eds.) Proc. Giant field
and new exploration concepts seminar, Indon. Assoc. Geol. (IAGI), Jakarta 2002, p. 1-5.
(Extended Abstract. Small 1996 discoveries in E Miocene Baturaja Fm limestones at Semoga 1, Kaji 1 and
Sembada 1 wells proved to be part of single large oil pool with recoverable reserves of ~200 MMBO. Oil below
structural spill points, demonstrating stratigraphic control on hydrocarbon accumulation)
Hwang, R.J., T. Heidrick, B. Mertani, Qivayanti & M. Li (2000)- Correlation and migration studies of North
Central Sumatra oils. Organic Geochem. 33, 12, p. 1361-1379.
(Tertiary lacustrine shale, Brown Shale, long recognized as main source rock for C Sumatra basin oils.
Biomarker and carbon isotopic data from producing fields indicate oils quite similar geochemically but several
genetic groups, tied to subtle differences in source facies)
Icke, H. & K.Martin (1907)- Over Tertiaire en Kwartaire vormingen van het eiland Nias. Samml. Geol. Reichs-
Mus. Leiden (1) 8, p. 204-252.
Bibliography of Indonesia Geology v. 4.1 47 www.vangorselslist.com July 2012