Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

(Banded Iron Formation deposits generally associated with sedimentary or meta-sedimentary rift basins in
Archaean- Precambrian cratons. Late Paleozoic ‘BIF-like’ meta-sedimentary rocks outcrop at Tanggamus,
Lampung, over narrow, >50 km belt along depositional strike, slightly parallel to main direction of Sumatra)
Subarya, C., M. Chlieh, L. Prawirodirdjo, J.P. Avouac, Y. Bock, K. Sieh et al. (2006)- Plate-boundary
deformation associated with the great Sumatra-Andaman earthquake. Nature 440, p. 46-51.
Subastedjo, M.T. & Sukarsono (1983)- Penyelidikan geologi untuk perencanaan tambang batubara dengan
contoh kasus perencanaan tambang batubara Muara Tiga, Bukit Asam Sumatra Selatan. Proc. 12th Ann. Conv.
Indon. Assoc. Geol. (IAGI), p. 209-213.
('Geological investigation for coal mine planning, with example of Muara Tiga mine, Bukit Asam, S Sumatra')
Subiyanto & H. Panggabean (2003)- Batuan terobosan dan pengaruhnya terhadap pematang batubara di daerah
Bukit Kendi, Tanjung Enim, Sumatra Selatan. J. Geol. Sumberdaya Min. (GRDC) 13, 134, p.
('Intrusive rocks and and their influence on coal seams in the Bukit Kendi area, Tanjung Enim, S Sumatra')
Subiyanto & H. Panggabean (2004)- Karakteristik pematangan dan peningkatan mutu batubara di daerah Bukit
Asam, Muara Enim, Sumatera selatan. Jurnal Sumber Daya Geol., GRDC Bandung, (14) 1, 1, p. 37-54.
(On the enhancement of Muara Enim Fm coal quality by igneous intrusions in Bukit Asam area, S Sumatra)
Subroto, E.A., R. Alexander, U. Pranyoto & R.I. Kagi (1992)- The use of 30-norhopanes series, A. Novel
carbonate biomarker in source rock to crude oil correlation in the North Sumatra Basin, Indonesia. Proc. 21st
Ann. Conv. Indon. Petrol. Assoc., I, p. 145-163.
(N Sumatra oils two groups: shaly and coaly, with distinct biomarker distributions. The 30-norhopanes as one
of carbonate biomarkers have been proposed recently. Three types of source rocks have been recognised in N
Sumatra Basin: shale, carbonaceous shale and calcareous shale. Recognition of three source types can only be
observed using hopane distribution. Crude oil of coaly shale type not found during this study)
Sudarsana, A. & E. Maulana (2000)- Factors affecting productivity in a shallow shoreface sandstone reservoir: a
case study from the Rebonjaro Field, South Sumatra Basin. Proc. 29 th Ann. Conv. Indon. Assoc. Geol. (IAGI),
Bandung, 1, p. 55-69.
(Oil productivity of very shallow A sand near top of M Miocene Lower Palembang Fm in 1929 field is better in
cross-bedded facies than in bioturbated facies)
Sudewo, B., A.R Suhendan & S. Chacko (1987)- Physical properties of carbonate reservoirs in South Sumatra.
Proc. 16 th Ann. Conv. Indon. Petrol. Assoc. 1, p. 363-383.
(Early Miocene Baturaja Lst in S Sumatra Basin significant oil- gas accumulation. Porosity varies widely
between tight platform facies and porous reefal facies. Seismic data may provide indirect evidence of porosity.
Iincreasing trend of acoustic impedance with depth is correlated with decrease in porosity, indicative of
compaction of limestones,)
Suhendan, A.R. (1984)- Middle Neogene depositional environments in Rambutan area, South Sumatra. Proc.
13th Ann. Conv. Indon. Petrol. Assoc.,1, p. 63-73.
(Miocene of Rambutan area, SW part of S Sumatra basin. Rambutan field oil in M Miocene Lower Palembang
Fm clastics)
Sukanta, U., Yarmanto, D. Kadar, H. Semimbar & D.A. Firminsyah (2008)- Current interpretation of regional
stratigraphy of Late Oligocene- Miocene Sihapas Group in the Central Sumatra Basin. In: Sumatra stratigraphy
workshop, Duri (Riau) 2005, Indon. Assoc. Geol. (IAGI), p. 81-82. (Abstract only)
(Summary of sequence stratigraphic study of C Sumatra Late Oligocene- E Miocene Sihapas Group. Five
lithostratigraphic units (old to young: Menggala, Bangko, Bekasap, Duri and Telisa Fms.). Seven basin-wide
sequence boundaries (SB 25.5, 22, 21, 17.5, 16.5, 15.5 and 13.8 Ma), bounding six 3 rd order sequences.
Younger sands mainly developed in N, NE and E of basin and Telisa shale best developed to W and SW,
suggesting sand sourced dominantly from N and NE, from Thailand-Malaysian Highs)
Bibliography of Indonesia Geology v. 4.1 95 www.vangorselslist.com July 2012