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Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

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Burton, D. & L.J. Wood (2010)- Interpreting the rift stratigraphy and petroleum systems elements <strong>of</strong> the West<br />

<strong>Natuna</strong> Basin using 3D seismic geomorphology. In: L.J. Wood et al. (eds.) Seismic imaging <strong>of</strong> depositional and<br />

geomorphic systems, Gulf Coast Sect. SEPM, Ann. Perkins Research Conf. 30, Houston, p. 376-395.<br />

Chalik, M. (2001)- Sealing and non-sealing faults along a major wrench trend in the Kakap area, West <strong>Natuna</strong><br />

Basin. Proc. 28th Ann. Conv. Indon. Petrol. Assoc., p. 757-778.<br />

Challis, M., R. Adhyaksawan & V. Ball (2006)- Seismic prediction <strong>of</strong> thin sand intervals for development<br />

drilling at North Belut Field, Block B, South <strong>Natuna</strong> Sea. Proc. Jakarta 2006 Int. Geosc. Conf. Exhib., Indon.<br />

Petrol. Assoc., Jakarta06-CH-06, 5 p.<br />

Dajczgewand, D. (2005)-Tectonic evolution and structural styles <strong>of</strong> deformation <strong>of</strong> southern Kakap Blocks,<br />

West <strong>Natuna</strong> Basin, <strong>Indonesia</strong>. In: Proc. 6th Congr. Exploracion y desarrollo de hidrocarburos, Mar del Plata,<br />

Argentina, 2005, 12p.<br />

(Structural evolution <strong>of</strong> Kakap oilfield area, W <strong>Natuna</strong> basin, based on work done in 2003 M.Sc Thesis at<br />

University <strong>of</strong> London. Extension started in Late Eocene, creating E-W trending half-graben with N-dipping<br />

normal faults. Second extensional phase began in M Oligocene. Compression started in latest Late Oligocene,<br />

initial stage being mild, and was stronger in E. Strongest compression/ tectonic inversion in M Miocene. Muda<br />

regional unconformity developed during late Middle Miocene and early Late Miocene and was subsequently<br />

deformed by compression, continuing to recent times)<br />

Daines, S.R. (1985)- Structural history <strong>of</strong> the West <strong>Natuna</strong> Basin and the tectonic evolution <strong>of</strong> the <strong>Sunda</strong><br />

Region. Proc. 14th Ann. Conv. Indon. Petrol. Assoc. 1, p. 39-61.<br />

(Structures in W <strong>Natuna</strong> Basin formed during two deformation periods: (1) extension from ~38-29 Ma,<br />

resulting in graben development in Boundary area; (2) compression, resulting in 2 stages basin inversion, 29-<br />

20 Ma left-lateral wrench movement and !5- 10 Ma when most NE-SW oil-bearing anticlines formed. Extensive<br />

Jurassic suture, separating Indochina and <strong>Sunda</strong>, responsible for propagation <strong>of</strong> Malay-<strong>Natuna</strong>-Lupar shear<br />

zone, and facilitated basin development in area)<br />

Darmadi,Y., E. Hartadi, B. Pangarso, I. Sihombing & R. Wijayanti (2011)- Reservoir characterization <strong>of</strong> the<br />

Gabus-1 reservoir in North Belut Field: an integration <strong>of</strong> core,well logs and seismic, <strong>Natuna</strong> Sea Basin,<br />

<strong>Indonesia</strong>. Proc. 35 th Ann. Conv. Indon. Petrol. Assoc., IPA11-G-196, 19p.<br />

(N Belut 1974 gas discovery with stacked sand reservoirs across 1700’ interval deposited in fluvio-deltaic<br />

environments in Oligo-Miocene Udang and Gabus formations. Gabus 1 interval two major sequences with<br />

sharp erosional base and shale on top. NNE-SSW trending incised valley system)<br />

Darmadi, Y, B.J. Willis & S.L. Dorobek (2007)- Three-dimensional seismic architecture <strong>of</strong> fluvial sequences on<br />

the low-gradient <strong>Sunda</strong> <strong>Shelf</strong>, Offshore <strong>Indonesia</strong>. J. Sedim. Res. 77, p. 225-238.<br />

(Sequence stratigraphy <strong>of</strong> Belida Field area, W <strong>Natuna</strong> Basin. Upper Muda Fm Pliocene-Holocene fluvial<br />

architecture study from high-resolution seismic. 225m dominantly fluvial section. Five main sequences <strong>of</strong><br />

episodic channel incision and bypass alternating with periods <strong>of</strong> floodplain aggradation)<br />

Dash, B.P. (1971)- Preliminary report on seismic refraction survey southeast <strong>of</strong> <strong>Natuna</strong> Islands and seismic<br />

pr<strong>of</strong>iling in the vicinity <strong>of</strong> the <strong>Natuna</strong> and Tioman Islands on the <strong>Sunda</strong> <strong>Shelf</strong>. United Nations ECAFE, 8th<br />

Session CCOP, p. 168-174.<br />

Dash, B.P., C.M. Shepstone, S. Dayal, S. Guru, B.L.A. Hains, G.A. King & G.A. Ricketts (1972)- Seismic<br />

investigations on the northern part <strong>of</strong> the <strong>Sunda</strong> shelf South and East <strong>of</strong> Great <strong>Natuna</strong> Island. United Nations<br />

ECAFE CCOP Techn. Bull. 6, p. 179-196.<br />

(Regional shallow seismic survey <strong>of</strong> 1160km, SE <strong>of</strong> Great <strong>Natuna</strong> island, showing basinal and ridge-like<br />

features. Khorat- <strong>Natuna</strong> swell may be linked with mainland Asia and NW Kalimantan)<br />

Dickerman, K.M. (1993)- The utilization <strong>of</strong> 3D seismic for small fields in the South <strong>Natuna</strong> Sea Block B. Proc.<br />

22nd Ann. Conv. Indon. Petrol. Assoc., 1, p. 659-678.<br />

<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 144 www.vangorselslist.com July 2012

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