Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
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Somantri, M. (2000)- Distribution <strong>of</strong> gamma-ray values and sulphur contents in relation with depositional<br />
environment <strong>of</strong> the coals in Bayunglincir coal area, South Sumatera. Proc. 29th Ann. Conv. Indon. Assoc. Geol.<br />
(IAGI), 1, p. 155-176.<br />
Sosromihardjo, S.P.C. (1988)- Structural analysis <strong>of</strong> the North <strong>Sumatra</strong> Basin- with emphasis on Synthetic<br />
Aperture Radar data. Proc. 17th Ann. Conv. Indon. Petrol. Assoc. 1, p. 187-209.<br />
Sosrowidjojo, I.B. (2006)- Coalbed methane potential in the South Palembang Basin. Proc. Jakarta 2006 Int.<br />
Geosc. Conf. Exhib., Indon. Petrol. Assoc., 06-CH-05, 5p.<br />
Sosrowidjojo, I.B., R. Alexander & R.I. Kagi (1994)- The biomarker composition <strong>of</strong> some crude oils from<br />
<strong>Sumatra</strong>. Organic Geochem. 21, p. 303-312.<br />
(Crude oils from N, C and S <strong>Sumatra</strong> basins analysed for biomarkers. Three types: (1) N <strong>Sumatra</strong> marine<br />
carbonate depositional setting (2) C <strong>Sumatra</strong> waxy crudes from brackish- lacustrine, and (3) light oil from N<br />
<strong>Sumatra</strong> and two oils from S <strong>Sumatra</strong> from deltaic/ nearshore depositional setting)<br />
Sosrowidjojo, I.B & F.X. Djatmiko (1997)- Petroleum system di Cekungan Sumatera Selatan, suatu kajian awal<br />
eksplorasi di sistem karbonat. Proc. 26th Ann. Conv. Indon. Assoc. Geol. (IAGI), Hydrocarbons, p. 50-57.<br />
('Petroleum system in the S Sumatr basin, some early exploration studies in the carbonate system')<br />
Sosrowidjojo, I.B., B. Setiardja, Zakaria, P.G. Kralert, R. Alexander & R.I. Kagi (1994)- A new geochemical<br />
method for assessing the maturity <strong>of</strong> petroleum: application to the South <strong>Sumatra</strong> Basin. Proc. 23rd Ann. Conv.<br />
Indon. Petrol. Assoc. 1, p. 439-455.<br />
(Assessing maturity <strong>of</strong> petroleum and source rocks using vitrinite reflectance and conventional biomarker data<br />
can be problematic when source rocks subjected to rapid heating and contain abundant land plant remains or<br />
when crude oil has been biodegraded. New maturity indicator based upon reactions <strong>of</strong> cadalene proposed)<br />
Sosrowidjojo, I.B. & A. Saghafi (2009)- Development <strong>of</strong> the first coal seam gas exploration program in<br />
<strong>Indonesia</strong>: reservoir properties <strong>of</strong> the Muaraenim Formation, South <strong>Sumatra</strong>. Int. J. Coal Geol. 79, p. 145-156.<br />
(Late Miocene Muaraenim Fm thick, low rank coals (lignite to sub-bituminous) in twelve named horizons.<br />
Believed most prospective for CBM production in <strong>Indonesia</strong>. Five exploration wells in Rambutan Gas field to<br />
~1000m depth. Five major coal seams between 450-1000 m. Coals vitrinite-rich (>75%). Gas contents in<br />
samples up to 5.8m3/t, mainly methane (CH4 80-93%, CO2 6 -19%). Gas released into production well richer<br />
in CH4 (94-98%). Suitable gas recovery parameters for three <strong>of</strong> five coal seams with total thickness <strong>of</strong> >30 m)<br />
Specht, T.D., T. Rahardjo, F.I. Frasse & P.B. Dobson (2000)- A comprehensive evaluation <strong>of</strong> the exploration<br />
potential <strong>of</strong> the Offshore Sibolga Area, West Coast <strong>Sumatra</strong> Island, <strong>Indonesia</strong>. AAPG Int. Conf. Exhib., Bali<br />
2000. (Abstract only)<br />
(Caltex Sibolga PSC in Mentawai Forearc Basin acquired in 1996. Water depths from onshore to >2000’;<br />
sediments up to ~20,000’ thick. Bordered by outer arc and Mesozoic-Paleozoic core and volcanic arc <strong>of</strong><br />
<strong>Sumatra</strong>. Basin began to subside around 17 Ma and received nearly continuous Neogene sedimentation.<br />
Regional right-lateral strike-slip faults produced differences in structural and stratigraphic evolution between<br />
sub basins. Shallow burial depths limit size <strong>of</strong> biogenic accumulations and low heatflow suggests only limited<br />
thermogenic petroleum system).<br />
Stankiewicz, J., T. Ryberg, C. Haberland, Fauzi & D. Natawidjaja (2010)- Lake Toba volcano magma chamber<br />
imaged by ambient seismic noise tomography. Geoph. Res. Lett. 37, L17306, 5 p.<br />
(Ambient noise tomography used to image low-velocity body representing magma chamber under Quaternary<br />
Lake Toba caldera. Chamber complex 3-D geometry, with at least two separate sub-chambers. Deep low<br />
velocity body below 7 km depth SW <strong>of</strong> lake possibly another magma chamber. <strong>Sumatra</strong> Fault marks velocity<br />
contrast, but only down to 5 k)<br />
Stevens, S.H. & G.F. Moore (1985)- Deformational and sedimentary processes in trench slope basins <strong>of</strong> the<br />
western <strong>Sunda</strong> Arc, <strong>Indonesia</strong>. Marine Geol. 69, 1-2, p. 93-112.<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 93 www.vangorselslist.com July 2012