Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Janele, P.T., T.H. Tankersley, G.H. Schmit, B.C. Wibowo, A. Rahardja H. & W.C. Dawson (2000)- Stochastic
modeling at Kotabatak Field, Central Sumatra Basin. Proc. 27th Ann. Conv. Indon. Petrol. Assoc., 19p.
(Kotabatak oil field modeling. NE-SW trending estuarine channels in Bekasap Fm reservoirs)
Jenkins, S.D., Hendar S.M. & E. J. Kodl (1994)- Integrated analysis of Petani gas sands in selected fields,
Central Sumatra. Proc. 23rd Ann. Conv. Indon. Petrol. Assoc. 1, p. 373-385.
(Seismic anomalies used to identify M-L Miocene Petani gas sands and allow areal mapping beyond the areas
of well control. Anomalies integrated with structure maps, sand isopach maps, facies maps and log gas
indications enable quick evaluation of small, shallow gas plays)
Jobson, D.H., C.A. Boulter & R.P.Foster (1994)- Structural controls and genesis of epithermal gold-bearing
breccias at the Lebong Tandai Mine, western Sumatra, Indonesia. J. Geochem. Expl. 50, p. 409-428.
(Lebong Tandai Neogene low-sulphidation, volcanic-hosted epithermal gold deposit in foothills of Barisan Mts)
Johansen, S. & H. Semimbar (2010)- Sand-rich tide-dominated deltaic systems of the Lower Miocene, Central
Sumatran Basin, Indonesia. AAPG Hedberg Conference, Jakarta 2009, Extended Abstract, 8p.
(online at: www.searchanddiscovery.net/documents/2010/50255johansen/ndx_johansen.pdf)
(C Sumatran Basin >100 oil-gas fields, mainly in E Miocene Sihapas Group sand-rich, tide-dominated deltaic
systems and updip fluvial equivalents. Preserved depositional systems tracts extend from updip fluvio-tidal
channels into delta-front inclined tidal-marine sands and muds, then into delta front deposits interbedded with
marine mudstones, sandy foram grainstones and cross-bedded glauconitic sands. Overall trend transgressive
and capped by marine shales)
Johari, S. (1988)- Geochemistry and tin mineralisation in northern Sumatra, Indonesia. In: C.S. Hutchison (ed.)
Tin mineralisation, with emphasis on Asian deposits. Springer Verlag, Heidelberg, p. 541-556
Jongmans, W.J. & W. Gothan (1925)- Beitrage zur Kenntnis der Flora des Oberkarbons von Sumatra. Verhand.
Geol. Mijnbouwk. Gen. Nederl. Kol., Geol. Ser., 8 (Verbeek volume), p. 279-303.
('Contibutions to the knowledge of the flora of the Upper Carboniferous of Sumatra'. First report on classic
Early Permian ‘Jambi flora’. 80 species, including 14 Pecopteris spp. Interpreted here as Upper Carboniferous
age, but subsequent papers all call it Permian) and of ‘European’ affinity, with no relations to Gondwana flora)
Jongmans, W.J. & W. Gothan (1935)- Die Ergebnisse der paläobotanischen Djambi-Expedition 1925. 2. Die
palaeobotanischen Ergebnisse. Jaarboek Mijnwezen Nederl. Indie (1930), 59, Verh. 2, p. 71-201.
('The results of the 1925 paleobotanic Jambi expedition'. Rich ‘Upper Carboniferous’ plant floras collected by
Tobler in Djambi many European affinities, no Gondwana elements. Later workers (van Waveren, etc.) reinterpreted
as Early Permian age, and confirmed Cathaysian affinity)
Jordan, C.F. & M. Abdullah (1988)- Lithofacies analysis of the Arun reservoir, North Sumatra. In: A.J.
Lomando & P.M. Harris (eds.) Giant oil and gas fields, a core workshop. SEPM Core Workshop 12, p. 89-117.
(Arun gas-condensate field in N Sumatra, producing from 1100' thick E-M Miocene reefal carbonate buildup.
Four facies associated with patch reef complexes. All facies in communication through microporous limestone.
Diagenetic reactions creating porosity far outweigh depositional controls on porosity distribution)
Jordan, C.F. & M. Abdullah (1992)- Arun Field- Indonesia North Sumatra Basin. AAPG Treatise Petroleum
Geology, Stratigraphic Traps III, p. 1-39.
(Arun largest gas field in N Sumatra basin, with initial dry gas in place of >16 TCF. Reservoir E-M Miocene
reefal buildup limestone)
Kadar, D., R. Preece & J.C. Phelps (2008)- Neogene planktonic foraminiferal biostratigraphy of Central
Sumatra Basin, Indonesia. In: Sumatra stratigraphy workshop, Duri (Riau) 2005, Indon. Assoc. Geol. (IAGI), p.
5-51.
(Six Late Oligocene- M Miocene planktonic foram zones in C Sumatra subsurface. Early M Miocene hiatus in
Minas and other fields, called Duri event, spans zone N10)
Bibliography of Indonesia Geology v. 4.1 49 www.vangorselslist.com July 2012