Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

(Three exploration wells at W edge C Sumatra Basin tested oil up to 3000 BOPD of 44 API oil in E Miocene
Lower Sihapas Fm sandstones. Low resistivity (6-8 Ohm m). Resistivity of Sihapas oil sands lower than older U
Pematang water sands, probably result of clay minerals in dispersed and laminated shale)
Setijadji, L.D. (2009)- Overview of the metallogeny of Sumatera. MGEI Bull. 1, p.
Setyobudi, E.B. (1982)- Batupasir Binio; lapisan pengandung gas dangkal di lapangan minyak Merbau (Riau).
Proc. 11th Ann. Conv. Indon. Assoc. Geol. (IAGI), p. 145-154.
('Binio sand: shallow gas trap in the Merbau oil field')
Setyobudi, E.B. & Solichin (1996)- Study of oil migration and remigration in the Southern Kampar Block,
Central Sumatra. Proc. 25th Ann. Conv. Indon. Petrol. Assoc. 1, p. 1-14.
(Small Paleogene Binio sub-graben between Lirik and Binio Fields likely source kitchen for Binio, Pekan and
Lirik Trend Fields. Sub-graben part of larger Bengkalis Trough. Major oil generation between ~10-8 Ma, when
Binio- Lirik Trend structures not yet formed. Hydrocarbons filled nearby paleo-structures, until Plio-
Pleistocene inversion tectonics caused spillage to present-day traps. Remaining exploration potential in subtle
folds in migration and remigration pathways)
Setyowiyoto, J. (1998)- Sedimentology of the Lower Sihapas Formation identified on conventional core data,
Bengkalis Trough. Proc. 27th Ann. Conv. Indon. Assoc. Geol. (IAGI), p. 146-158.
Shaw, J.H., S.C. Hook & E.P. Sitohanh (1997)- Extensional fault-bend folding and synrift deposition: an
example from the Central Sumatra Basin, Indonesia. AAPG Bull. 81, 3, p. 367-379.
(Geometry and structural history of Paleogene half-grabens)
Shell Mijnbouw (1978)- Geological map of the South Sumatra coal province, 1:250,000. (Unpublished)
Sibuet, J.C., C. Rangin, X. Le Pichon, S.C. Singh, A. Cattaneo, D. Graindorge, F. Klingelhoefer, J.Y. Lin, J.
Malod et al (2007)- 26th December 2004 Great Sumatra-Andaman earthquake: seismogenic zone and active
splay faults. Earth Planet. Sci. Lett. 263, p. 88-103.
Sieh, K. & D. Natawidjaja (2000)- Neotectonics of the Sumatran fault, Indonesia. J. Geophys. Res. 105, p.
28,295-28,326.
Siemers, C.T. & R.A. Lorentz (1992)- Sedimentological/petrological analysis of reservoir units within the
fluvial/estuarine/marine depositional complex of the Talang Akar Formation (Oligocene), Bentayan Field,
South Sumatra, Indonesia. AAPG Int. Conf., Sydney 1992, Search and Discovery Article #91015. (Abstract
only) (Bantayan field NW trending anticlinal structure on NE flank of S Sumatra basin.1932 discovery in upper
Talang Akar sandstones. Up to 12 potentially productive sandstone units. Six main fluvial- shallow marine
reservoir intervals, of variable quality. Stacked fluvial channel braidplain deposits are only ones with good
reservoir potential; channel-fills tend to merge into well-connected braidplain type reservoir system)
Silitonga, P.H. & D. Kastowo (1975)- Geologic map of the Solok Quadrangle, Sumatra (5/VIII) 1:250,000.
Geol. Res. Dev. Centre, Bandung, 8p. + map
Silvestri, A. (1925)- Sur quelques foraminiferes et pseudoforaminiferes de Sumatra. Verhand. Geol.-
Mijnbouwk. Gen. Nederl. Kolon., Geol. Ser. 8 (Verbeek volume), p. 449-458.
('On some foraminifera and pseudoforaminifera from Sumatra'. Foraminifera from Cretaceous limestones from
Sungi Tuo (Korinci, Jambi) with Choffatella (= Pseudocyclammina; Yabe 1943) and Gumai Mts Saling series
with Lacazina (=Loftusia))
Silvestri, A. (1932)- Revisione di foraminiferi preterziarii del Sud-Ouest di Sumatra. Riv. Ital. Pal. 38, p. 75-
107.
Bibliography of Indonesia Geology v. 4.1 89 www.vangorselslist.com July 2012