Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Feriyanto, F. Kamil, Y. Kusnandar & Y. Yanto (2005)- Successful identification of thin carbonate on paleobasement
high: special case in Palembang High, South Sumatra Basin. Proc. 30 th Ann. Conv. Indon. Petrol.
Assoc., 1, p. 91-100.
(On seismic recognition of thin Baturaja Fm buildups on Palembang High, S Sumatra)
Finger, K.L. & W.S. Drugg (1992)- Microfossils as indicators of deltaic subenvironments, Minas Field, Central
Sumatra. Proc. 21st Ann. Conv. Indon. Petrol. Assoc., 1, p. 225-237.
(Depositional environments of E Miocene Bekasap Fm interpreted as fluvial delta plain to distal delta front or
prodelta. Biotic distributions controlled primarily by salinity and pH gradients. Association of large coastal
foraminifera with minute deeper water forms implies shoreward transport of latter and supports concept of
tide-dominated Bekasap delta)
Firmansyah D.A., A. Rifai, S. Yudho, A. Kamal & R.M.I. Argakoesoemah (2007)- Exploring shallow prospects
in Iliran Basement High, South Sumatra Basin. Proc. 31 st Ann. Conv. Indon. Petrol. Assoc. IPA07-G-141, 10 p.
(Hydrocarbon exploration in Iliran High region since early 1900s, when heavy oil was produced from shallow
wells around asphalt, oil and gas seeps. Down flank discoveries W Iliran and S Tabuan in 1980s. Iliran High
remained high since Late Oligocene and focal point for hydrocarbon migration since Late Miocene. Plio-
Pleistocene tectonics resulted in tilting to SW. Three exploration plays: crest-structure, down-flank, and
fractured basement. Prospects all < 2500’, and seal highest risk)
Fitch, T.J. (1972)- Plate convergence, transcurrent faults, and internal deformation adjacent to Southeast Asia
and the western Pacific. J. Geophys. Res. 77, p.4432-4460.
Fitrianto, T., H.N. Saputra, B. Syam & A.H. Purwanto (2012)- The origin, distribution and prediction of CO2 in
South Sumatra, a case study: Jabung Block and surrounding area. Proc. 36th Ann.Conv. Indon. Petrol. Assoc.,
Jakarta, IPA12-G-025, p. 1-10.
(Several gas discoveries in S Sumatra Jabung, South Jambi and Corridor Blocks CO2 contents 40%- 90% CO2
or more. Carbon isotopes in Jabung area suggest origin of CO2 mainly from inorganic mantle degassing, with
minor contribution from thermal breakdown of kerogen and carbonate)
Fletcher, G. & Yarmanto (1993)- Post-Convention fieldtrip 1993- Ombilin Basin, West Sumatra. Indon. Petrol.
Assoc., 71 p.
Fliegel, G. (1901)- Uber Oberkarbonische Faunen aus Ost und Sudasien. I. Oberkarbonische Fauna von Padang.
Palaeontographica 48, 2-3, p. 91-136.
('On Upper Carboniferous faunas from East and South Asia, 1. Upper Carboniferous of Padang')
Fontaine, H. (1983)- Some Permian corals from the Highlands of Padang, Sumatra, Indonesia. Publ. Geol. Res.
Dev. Centre, Bandung, Paleont. Ser. 4, p. 1-31.
(Middle Permian reefal limestone from Guguk Bulat and Silungkang areas E of Singkarak lake, C Sumatra.
Coral faunas include Wentzelloides, etc., and similar to those from mainland SE Asia)
Fontaine, H. (1986)- Microfacies of a few Permian limestones of Sumatra, Peninsular Malaysia and Thailand.
United Nations CCOP Techn. Bull. 18, p. 148-157.
(Incl. photomicrographs of Permian foram-algal grainstones-packstones and oolitic limestone from Jambi
Province)
Fontaine, H. (1986)- Discovery of Lower Permian corals in Sumatra. In: G.H. Teh & S. Paramananthan (eds.)
Proc. GEOSEA V Conf., Kuala Lumpur 1984, 1, Geol. Soc. Malaysia Bull. 19, p.183-191.
(First record of E Permian corals from Sumatra, in Jambi Province (Pulau Apat, Muara Liso, Batu Gajah, Batu
Impi). Associated with M-L Asselian Pseudoschwagerina zone fusulinids. Lower Permian sediments well
developed in upper Mesumai River area and represent forested volcanic arc surrounded by shallow sea)
Bibliography of Indonesia Geology v. 4.1 30 www.vangorselslist.com July 2012