Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Dunn, P.A., M.G. Kozar & Budiyono (1996)- Application of geoscience technology in a geologic study of the
Natuna gas field, Natuna Sea, offshore Indonesia. Proc. 25 th Ann. Conv. Indon. Petrol. Assoc. 1, p. 117-130.
Eric, M. & A. Hendro (1996)- The petroleum systems of west Block 'B' PSC, South Natuna Sea, Indonesia.
Proc. 25th Ann. Conv. Indon. Petrol. Assoc, 1, p. 465-479.
Evans, H. (1998)- New life in an old basin, an example from Natuna Sea Block A. In: Proc. SEAPEX Expl.
Conf. OFFSEA 98, Singapore 1998, p. 141-154.
Eyles, D.R. & J.A. May (1984)- Porosity mapping using seismic interval velocities, Natuna L structure. Proc.
13 th Ann. Conv. Indonesian Petrol. Assoc., p. 301-316.
Fachmi, M. & L.J. Wood (2005)- Seismic geomorphology: a study from West Natuna Basin, Indonesia. Proc.
30 th Ann. Conv. Indon. Petrol. Assoc., 1, p. 163-
(Two types of U-M Miocene fluvial/ fluvial-deltaic systems can be identified on 3D seismic horizon slices from
Belanak and Gabus areas in W Natuna basin: a meandering river system and distributary channel system)
Fahman, M., Faisal Nur, J.S. Djalal, Subagio & Kasjati (1991)- An overview of the Anoa field development.
Proc. 20 th Ann. Conv. Indon. Petrol. Assoc., p. 293-313.
Fainstein, R. & J. Meyer (1997)- Structural interpretation of the Natuna Sea, Indonesia. SEG 1997 Conv.
Abstract, p. 639-642.
(W Natuna Basin extensional episodes in Eocene and Oligocene, followed by compression/ inversion peaking in
Late Miocene, with oil fields in syn-rift clastics and inversion anticlines. East Natuna basin major features are
Miocene carbonate buildups)
Fairburn, J.R. (1994)- Conoco Belida Field- directional driling case study. Proc. 23rd Ann. Conv. Indon. Petrol.
Assoc. Jakarta 1994, 2, p. 315-325.
Franchino, A. (1990)- Notes sur les Iles Natuna. Archipel 39, p. 47-63.
('Notes on the Natuna islands'. Mainly geographic description with notes and map on geology. Core of island
E-W trending high composed of Jurassic- Cretaceous sediments and volcanics of Bunguran Beds, with cherts
and gabbros-serpentinites. Late Cretaceous granite intrusions, the largest Mount Ranai (1035m). Overlain by
Oligocene Natuna Sandstone)
Franchino, A. & P. Liechti (1983)- Geological notes on the stratigraphy of the island of Natuna, Indonesia.
Mem. Scienze Geol. (Padova) 36, p. 171-193.
Franchino, A. & C. Viotti (1986)- Stratigraphic notes on Middle Miocene-Recent sequence in East Natuna
Basin (Indonesia). Mem. Scienze Geol. (Padova) 38, p. 111-127.
Gaynor, J., G. Hepler & M. Thornton (1995)- the importance of reservoir characterization and sedimentology in
the Belida Field development. Proc. 24th Ann. Conv. Indon. Petrol. Assoc. 2, p. 361-375.
(On reservoir characterization of 214 MMBO Belida Field. Oil in two major units separated by 200’ thick
Barat shale: Oligocene Udang Fm fine-grained in lacustrine delta sandstone, and E Miocene Lower Arang Fm
m-grained tide dominated marine shelf sandstones)
Ginger, D.C., W.O. Ardjakusumah, R.J. Hedley & J. Pothecary (1993)- Inversion history of the West Natuna
Basin: examples from the Cumi-Cumi PSC. Proc. 22nd Ann. Conv. Indon. Petrol. Assoc. I, p. 635-658.
(W Natuna Basin similar to many Sundaland basins with Late Eocene- E Oligocene extension creating complex
system of rift basins. From earliest Miocene times basins progressively inverted in right-lateral stress regime.
Wrench zones also developed by reactivation of NW-SE faults in earlier rift system. Displacement across faults
Bibliography of Indonesia Geology v. 4.1 145 www.vangorselslist.com July 2012