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Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

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Wagimin, N. & E.A. Sentani (2009)- Opportunities (II), East <strong>Natuna</strong> area. Inameta J. 7, p. 24-27.<br />

(online at: www.patranusa.com)<br />

(Brief overview <strong>of</strong> E <strong>Natuna</strong> Basin, in conjunction with tender round <strong>of</strong>fering)<br />

Wirojudo, G.K. & A. Wongsosantiko (1985)- Tertiary tectonic evolution and related hydrocarbon potential in<br />

the <strong>Natuna</strong> area. Energy 10, 3/4, p. 433-455.<br />

Wongkosantiko, A. & P. Prijosoesilo (1995)- Geologic summary <strong>of</strong> the <strong>Natuna</strong> Sea. In: Seismic Atlas <strong>of</strong><br />

<strong>Indonesia</strong>n Oil and Gas Fields, II: Java, Kalimantan, <strong>Natuna</strong>, Irian Jaya, Indon. Petrol. Assoc., Jakarta, 6p.<br />

Wongkosantiko, A. & G.K. Wirojudo (1984)- Tertiary tectonic evolution and related hydrocarbon potential in<br />

the <strong>Natuna</strong> area. Proc. 13 th Ann. Conv. Indon. Petrol. Assoc., p. 161-183.<br />

(W and E <strong>Natuna</strong> Basins separated by N-S trending <strong>Natuna</strong> basement Arch. W <strong>Natuna</strong> Basin started in E<br />

Oligocene by rifting/ pull-apart, producing SW-NE half-grabens filled with non-marine sediments. Extension in<br />

W <strong>Natuna</strong> little effect on E <strong>Natuna</strong> Basin, where Oligocene sediments more uniform thickness. Compressive<br />

forces started in W <strong>Natuna</strong> in E Miocene, resulting in inversions <strong>of</strong> former half grabens)<br />

<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 152 www.vangorselslist.com July 2012

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