Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Prasetyo, H., E. Suparka & D. Noeradi Darussalam (2009)- Characterization of low-permeability reservoir rock
using petrography and depositional studies- case study: optimizing production from low-permeability Bekasap
Sandstones in Central Sumatra, Indonesia. AAPG Int. Conf. Exh., Rio de Janeiro 2009, Search and Discovery
Article #40513 (2009), 13p. (Extended Abstract)
(E Miocene Bekasap Fm sandstone reservoirs in C Sumatra basin deposited in estuarine, tide-dominated delta
system. Overall fining-upward: lower part m- grained, conglomeratic, cross-bedded and massive sandstones,
with permeability up to 1900 mD, upper part f-vf-grained, bioturbated sandstone with permeability from 10's-
200 mD. In general, reservoir quality more controlled by depositional environment than diagenetic processes.
At depth both permeability and porosity reductions significantly controlled by cementation)
Pratiwi, F.I., V.B. Indranadi & B. Toha (2011)- Sequence stratigraphy for facies modeling of Upper Lakat and
Tualang Formation: implication for Late Oligocene to Early Miocene paleogeography of southern Bengkalis
Trough. Proc. Joint 36 th HAGI and 40th IAGI Ann. Conv., Makassar, JCM2011-225, 12p.
(Sequence stratigraphy of Late Oligocene-E Miocene fluvial- tidal channel reservoir intervals in field 'X'
(probably Stanvac Kayuara field; HvG), at S end Bengkalis Trough, C Sumatra Basin. Sands quartz-rich and
derived from N-NE part of Bengkalis, from Malacca Terrane basement high)
Prawirodirdjo, L., Y. Bock, J.F. Genrich, S.S.O. Puntodewo et al. (2000)- One century of tectonic deformation
along the Sumatran fault from triangulation and Global Positioning System surveys. J. Geophys. Res. 105, p.
28,343-28,361.
(Analysis combining historical triangulation and recent GPS measurements in W and N Sumatra reveals
detailed slip history along central part of Sumatran fault)
Prawirodirdjo, L., Y. Bock, R. McCaffrey, J. Genrich, E. Calais et al. (1997)- Geodetic observations of
interseismic strain segmentation at the Sumatra subduction zone. Geophys. Res. Lett. 24, 21, p. 2601-2604.
(GPS suggests complete coupling of forearc to subducting plate S of 0.5°S, half as much to N)
Prayitno, W., J.W. Armon & S. Haryono (1992)- The implications of basin modeling for exploration- Sunda
Basin case history, offshore southeast Sumatra. Proc. 21st Ann. Conv. Indon. Petrol. Assoc., p. 379-416.
Premonowati (2011)- Outcrops conservation of Tanjung Baru or Lower Talang Akar Formation, Baturaja city
of Palembang area - South Sumatra Basin: how important? Berita Sedim. 20, p. 7-11.
(online at: http://www.iagi.or.id/fosi/bs20-sumatra.html. Proposal to conserve quarry in Late Oligocene or
basal Miocene fluvial conglomeratic quartz sst of Gritsand Mb of Lower Talang Akar Fm E of Baturaja, with
proposal to rename into Tanjung Baru Fm. With overview of stratigraphy of this part of S Sumatra basin)
Priwastono, D., A. Kohar, J. Layundra & D. Wanengpati (2005)- The seismic characteristics of the Langsa L
carbonate build-up, the first offshore oil production in Nanggroe Aceh Darussalam Province. Proc. 30 th Ann.
Conv. Indon. Petrol. Assoc., IPA05-G-171, 10p.
(L oil field discovered in 1980 by Mobil in Malacca Straits. Reservoir Early Miocene Malacca Fm carbonate
buildup with av. porosities 6.4- 10.7%)
Priyomarsono, S. & A. Sumarsono (1993)- Tektonik geologi daerah pegunungan Tigapuluh dan daerah
sekitarnya, cekungan Sumatra selatan. Proc. 22nd Ann. Conv. Indon. Assoc. Geol. (IAGI), 1, p. 103-111.
(Tectonics of Tigapuluh Mountains and surrounding area, S Sumatra Basin)
Pubellier, M., C. Rangin, J.P. Cadet, I. Tjashuri, J. Butterlin & C. Mueller (1992)- Lile de Nias, un edifice
polyphase sur la bordure interne de la fosse de la Sonde (Archipel de Mentawai, Indonesie). C.R. Acad. Sci.,
Ser. II, 8, p. 1019-1026.
(Nias Island classically regarded as emergent accretionary wedge. Complex belt affected by polyphase
tectonics in Eocene and M Miocene. Sediments shelf clastics and limestone. Nias Melange extremely thin
mylonites and olistostromic scaly clay at several decollement levels. Reactivation of Eocene Tethys suture zone
within crustal blocks of Sunda margin could be alternative hypothesis for structure of Mentawai Islands)
Bibliography of Indonesia Geology v. 4.1 79 www.vangorselslist.com July 2012