Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

(Broad Oligo-Miocene paleogeographic map of N Sumatra onshore, E of Barisan Range, between Tamiang
River to N and Toba-Asahan River to S. Eo-Oligocene sediments in NE Sumatra basin 5000-7000 m thick. With
discussion of N Sumatra geology and stratigraphy
Adiwidjaja, P. & G.L. de Coster (1973)- Pre-Tertiary paleotopography and related sedimentation in South
Sumatra. Proc. 2nd Ann. Conv. Indon. Petrol. Assoc., p. 89-103.
Adlan, F. (2006)- Potensi hidrokarbon prospek dalam pada lapangan-lapangan tua di sub-cekungan Palembang
bagian Selatan. Proc. 35th Ann. Conv. Indon. Assoc. Geol. (IAGI), Pekanbaru 2006, 7 p.
(‘Hydrocarbon prospects in old fields in S part of Palembang sub-basin’. Ten old oil fields on Pendopo-Limau
anticlinorium with 1340 MMBO oil and 3 TCF gas in place. Additional prospects remaining in this trend)
Aernout, W.A.J. (1927)- Enkele nieuwere gegevens over de ertsafzettingen van Salida. De Mijningenieur 8, p.
73-76.
('Some new data on the ore deposits of Salida', W Sumatra gold-silver mine)
Agus, A. Subandrio, S. Widada, Feriyanto, S. Rakimi & Wibisono (2005)- Carbonate development on the TN
field in the Lematang Trough, South Sumatra basin. Proc. 13 th Ann. Conv. Indon. Petrol. Assoc., 1, 13 p.
(TN 1997 gas discovery in Baturaja Fm carbonate buildup on local high in Lematang Trough at ~12,000’
depth, and tested 30.7 MMSCFD from 250’ gross interval. Reef complex elongated, NNE-SSE trending, area
18.8 km2 and relief approximately 600’. Carbonate porosity average 6.8-9.6%, moldic/ vuggy and
intercrystalline, microfracture type porosity in several areas with permeability between 0.32-1.7 mD)
Akbar, M., B. Vissapragada, A.H. Alghamdi, D. Allen et al. (2001)- A snapshot of carbonate reservoir
evaluation. Oilfield Review, Schlumberger, Winter 2000/2001, p. 20- 41.
(online at: http://www.slb.com/~/media/Files/resources/oilfield_review/ors00/win00/p20_41.ashx)
(Reservoir evaluation paper with example of M Miocene buildup in Sibolga basin, off NW Sumatra, with
unsuccessful 1997 well due to lack of internal seals and late top seal preventing capture of early biogenic gas)
Akuanbantin, H. & D. Ardiputra (1976)- Geology of East Benakat oil field, South Sumatra. Proc. 5 th Ann.
Conv. Indon. Petrol. Assoc., 1, p. 59-68.
(East Benakat first drilled in 1930, testing minor oil in Talang Akar Fm of NW-SE trending anticline.
Renewewed interest and development decision after Pertamina drilled E Benakat 3 in 1973)
Alamsyah, M.N., S. Marmosuwito, W. Sutjiningsih, L.P. Marpaung & S. Sukmono (2008)- Seismic reservoir
characterization of Indonesia's Southwest Betara Field. The Leading Edge 27, 12, p. 1598-1607.
(SW Betara Field 2005 PetroChina discovery in Talang Akar Fm of Jabung Block, S Sumatra)
Alamsyah, M.N., A. Wasono Aji, Sihman M., B. Wisnu H. et al. (2006)- Reservoir characterization study to
determine thin sand reservoirs using AVO Inversion and spectral decomposition analysis, 3D onshore seismic
data of Ripah Field. Proc. Jakarta 2006 Int. Geosc. Conf. Exhib., Indon. Petrol. Assoc., 06-RC-04, 6p.
(Identification of Late Oligocene Talang Akar Fm NNE trending deltaic channel sands in 2000 Ripah field,
Jabung Basin, S Sumatra)
Aldiss, D.T. & S.A. Ghazali (1984)- The regional geology and evolution of the Toba volcanotectonic
depression, Indonesia. Quart. J. Geol. Soc. 141, 3, p. 487-500.
(Sumatra Late Quaternary Toba volcano-tectonic depression largest resurgent cauldron and one of largest
ignimbrite fields (Toba Tuffs: 3000 km3 of acid tuffs over 20,000 km2). Greater part of Toba Tuffs single
ignimbrite cooling unit, formed ~100,000 years ago. Toba depression formed after lithification of Toba Tuffs
by collapse along regional faults. Resurgent uplift raised lake sediments in depression by 500 m. Eruption of
Toba Tuffs and post-ignimbrite volcanism on line of W marginal fault of depression. This marginal fault once
extended N offshore into zone of Miocene back-arc rifting)
Bibliography of Indonesia Geology v. 4.1 6 www.vangorselslist.com July 2012