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Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

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Sitompul, N., Rudiyanto, A. Wirawan & Y. Zaim (1992)- Effects <strong>of</strong> sea level drops during Late Early Miocene<br />

to the reservoirs in South Palembang sub Basin, South <strong>Sumatra</strong>, <strong>Indonesia</strong>. Proc. 21st Ann. Conv. Indon. Petrol.<br />

Assoc. 1, p. 309-324.<br />

(Late Early Miocene sea level drops form sequence boundaries in late N6 and late N7. SB in Late N6 in Lower<br />

Talang Akar Fm, forming thick sand bodies which could be reservoirs. Late N7 sea level drop produced<br />

secondary porosity for carbonate reservoirs)<br />

Situmeang & P.R. Davies (1986)- A geochemical study <strong>of</strong> Asameras Block A Production Sharing Contract,<br />

North <strong>Sumatra</strong> Basin. Proc. 15th Ann. Conv. Indon. Petrol. Assoc., p. 321-340.<br />

(N <strong>Sumatra</strong> Block "A" with 11 commercial oil fields, which produced over 100 MBO, and one non-commercial<br />

gas field at Alur Siwah. In E part <strong>of</strong> block kerogen characterized by abundant land-derived organic material,<br />

while marine sapropelic organic matter increases to W, suggesting influx <strong>of</strong> land- derived organic matter from<br />

eastern land mass in area <strong>of</strong> Malacca Straits. Oils from Keutapang and Seureula Fm reservoirs <strong>of</strong> six different<br />

fields typically non-waxy, paraffinic, with 49.2° - 59°API gravities. Oils have common origin, probably fine<br />

grained marine sediments <strong>of</strong> M-L Miocene Baong Fm)<br />

Situmeang, S.P., C.W. Zeliff & R.A. Lorents (1992)- Characterization <strong>of</strong> low relief carbonate banks, Baturaja<br />

Formation, Ramba A and B pools, South <strong>Sumatra</strong>, <strong>Indonesia</strong>. In: C.T. Siemers et al. (eds.) Carbonate rocks and<br />

reservoirs <strong>of</strong> <strong>Indonesia</strong>: a core workshop. <strong>Indonesia</strong>n Petrol. Assoc., p 8.1 - 8.10.<br />

(Ramba Field produced 60 MBO oi1 1982-1992 from A and B pools, separated by paleochannel. Best reservoir<br />

rocks coral-rich packstones- wackestones, with 16-18% porosity)<br />

Situmorang, B., N.A. Harbury & M.G. Audley-Charles (1987)- Tectonic inversions in the <strong>Sunda</strong> Forearc:<br />

evidence from Simeulue. Proc. 16th Ann. Conv. Indon. Petrol. Assoc. 1, p. 57-63.<br />

(Cenozoic history <strong>of</strong> Simeulue, NW <strong>of</strong> Nias, includes Oligo-Miocene erosional unconformity. Repeated tectonic<br />

inversions may be related in part to transpression and transtension stresses generated by strike-slip motion<br />

interacting with sinuosities in trench and <strong>Sumatra</strong>n fault system)<br />

Situmorang, B. & Soepatono (1975)- Results <strong>of</strong> petroleum exploration in the interdeep basin <strong>of</strong>f West <strong>Sumatra</strong><br />

<strong>Indonesia</strong>. Proc. 12th Sess. CCOP, p. 255-262.<br />

Situmorang, B., S Wijaya, M. Husen & B. Yulihanto (1990)- Analisis struktur geologi Pulau Nias. Proc. 19th<br />

Ann. Conv. Indon. Assoc. Geol. (IAGI), 2, p. 27-41.<br />

('Analysis <strong>of</strong> the structure <strong>of</strong> Nias island')<br />

Situmorang, B. & B. Yulihanto (1985)- The role <strong>of</strong> strike slip faulting in structural development <strong>of</strong> the North<br />

<strong>Sumatra</strong> Basin. Proc. 14th Ann. Conv. Indon. Petrol. Assoc. 1, p. 21-38.<br />

(N <strong>Sumatra</strong> Basin development controlled by strike slip faulting. Several major N-S trending strike slip faults<br />

mainly with dextral movements formed in present back-arc region and arranged in en echelon pattern. Since<br />

then and until M Miocene, basin characterized by normal faulting. This episode corresponds to change in<br />

Indian Ocean spreading direction from N-S in E Paleogene to NE-SW. Convergence highly oblique in Late<br />

Miocene, producing compressive deformation and uplift. Compressional structures continuously affected<br />

sedimentary cover in Plio-Pleistocene due to strike slip faulting along <strong>Sumatra</strong>n Fault system)<br />

Situmorang, B. & B. Yulihanto (2007)- Formation <strong>of</strong> pull-apart basin along transcurrent fault: lesson from<br />

Sumatera. In: Geologi <strong>Indonesia</strong>: dinamika dan produknya, Geol. Res. Dev. Centre, Bandung, Spec. Publ. 33,1,<br />

p. 29-48.<br />

(Two prominent NW-SE transcurrent fault zones in <strong>Sumatra</strong>: Sumatera FZ parallel to the axis <strong>of</strong> the Barisan<br />

Mountains and Mentawai FZ along E slope <strong>of</strong> fore-arc ridge. N <strong>of</strong> Nias, MFZ and SFZ are linked by Batee<br />

Fault. Transtentional basins in back-arc (N, C, S <strong>Sumatra</strong>, Ombilin) and fore-arc (Singkel, Pini in NW, Bose,<br />

Sipora grabens in Mentawai area and Pagarjati, Kedurang in Bengkulu to SE).<br />

Situmorang, B., B. Yulihanto, A. Guntur, R. Himawan & G. J. Jacob (1991)- Structural development <strong>of</strong> the<br />

Ombilin basin, West <strong>Sumatra</strong>. Proc. 20st Ann. Conv. Indon. Petrol. Assoc.p. 1-15.<br />

<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 91 www.vangorselslist.com July 2012

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