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Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

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Kadir, W.G.A., S. Sukmono, M.T. Zen, L. Hendrajaya & D. Santoso (1996)- Gravity evidence for the thinning<br />

<strong>of</strong> the crust around the North <strong>Sumatra</strong> area. Proc. 25 th Ann. Conv. Indon. Petrol. Assoc., p. 81-91.<br />

(Structural discontinuity around N <strong>Sumatra</strong> effect <strong>of</strong> split in descending oceanic plate along continuation <strong>of</strong><br />

Investigator Ridge Transform Fault. Discontinuity reflected by sharp change <strong>of</strong> <strong>Sumatra</strong> Fault, volcanic line<br />

<strong>of</strong>fset and major changes to strike <strong>of</strong> Batee fault and Batee trench. Area around discontinuity low gravity<br />

anomaly with higher anomaly in center, indicating low density body <strong>of</strong> mantle material intruded by higher<br />

density igneous material in center. Gravity model pattern reflects thinning <strong>of</strong> crust beneath N <strong>Sumatra</strong> due to<br />

regional tensional stresses <strong>of</strong> mantle depth at ~20 km depth)<br />

Kalan, T., R.J. Maxwell & J.H. Calvett, (1984)- Ramba and Tanjung Laban oil discoveries, Corridor Block,<br />

South <strong>Sumatra</strong>. Proc. 13 th Ann. Conv. Indon. Petrol. Assoc., 1, p. 365-384.<br />

(Two oil discoveries in E Miocene Baturaja Limestone reservoirs. Ramba 1 with 57m reefal limestone, average<br />

porosity 19%, Tanjung Laban 1 has 63m limestone, 18m oil pay)<br />

Kallagher, H.J. (1989)- The structural and stratigraphic evolution <strong>of</strong> the <strong>Sunda</strong> Forearc Basin, North <strong>Sumatra</strong>.<br />

Ph.D. Thesis Univ. London, 387 p.<br />

Kamal, A. (2000)- Hydrocarbon potential in the Pasemah Block, a frontier area in South <strong>Sumatra</strong>. Proc. 27th<br />

Ann. Conv. Indon. Petrol. Assoc., 1, p. 49-63.<br />

(Pasemeh Block is small intra-montane basin near Pageralam in Barisan Mts, behind Gumai Mts. Miocene<br />

stratigraphy with Talang Akar quartz sandstones and baturaja Limestone suggests it was western extension <strong>of</strong> S<br />

<strong>Sumatra</strong> basin. Surface oil and gas seeps and thermogenic hydrocarbons (incl. high-CO2 gas) in first<br />

exploration well Ruas-1 suggest working petroleum system in Muara Dua area in SE <strong>of</strong> block. Quality <strong>of</strong><br />

seismic data poor, due to presence <strong>of</strong> young near-surface volcanics)<br />

Kamal, A., R.M.I. Argakoesoemah & Solichin (2008)- A proposed basin-scale lithostratigraphy for South<br />

<strong>Sumatra</strong> Basin. In: <strong>Sumatra</strong> stratigraphy workshop, Duri (Riau) 2005, Indon. Assoc. Geol. (IAGI), p. 85-97.<br />

(Description <strong>of</strong> Eocene- Pliocene stratigraphy <strong>of</strong> S <strong>Sumatra</strong> basin)<br />

Kamili, Z.A. & A.M. Naim (1973)- Stratigraphy <strong>of</strong> Lower and Middle Miocene sediments in North <strong>Sumatra</strong><br />

Basin. Proc. 2 nd Ann. Conv. Indon. Petrol. Assoc., p. 53-72.<br />

(Discussion <strong>of</strong> stratigraphy and facies <strong>of</strong> E Miocene <strong>of</strong> NE <strong>Sumatra</strong> basin)<br />

Kamili, Z.A., A. Wahab, J. Kingston, Z. Achmad, S. Sosromihardjo & C.U. Crausaz (1976)- Contribution to the<br />

Pre-Baong stratigraphy <strong>of</strong> North <strong>Sumatra</strong>. Proc. 5 th Ann. Conv. Indon. Petrol. Assoc., p. 91-108.<br />

Karig, D.E., M.K. Lawrence, G.F. Moore & J.R. Curray (1980)- Structural framework <strong>of</strong> the fore-arc basin,<br />

NW <strong>Sumatra</strong>. J. Geol. Soc. London 137, p. 77-91.<br />

(<strong>Sumatra</strong> fore-arc basin subsiding trough between rising subduction complex and elevated continental core. Up<br />

to 4 km <strong>of</strong> Miocene-Recent on E flank <strong>of</strong> basin over unconformity cut across Paleogene continental margin that<br />

was uplifted and disrupted in Late Oligocene. Large step-like <strong>of</strong>fsets <strong>of</strong> paleo-shelf edge attributed to rightlateral<br />

strike-slip faults, splaying across fore-arc from <strong>Sumatra</strong> Fault Zone. Offsets up to 100 km+, producing<br />

marginal re-entrants that became sites <strong>of</strong> turbidite-filled basins behind growing Neogene accretionary prism.<br />

Larger re-entrants may be floored with oceanic crust. Seaward flank <strong>of</strong> fore-arc basin migrated W during<br />

Neogene subduction. By late M Miocene, trench slope break was near sea level and formed shelf edge high.<br />

Thrusting and folding related to subduction probably decreased gradually upslope until LatePliocene, when<br />

large flexures and E-directed reverse faults developed)<br />

Karig, D.E., G.F. Moore, J.R. Curray & M.B. Lawrence (1980)- Morphology and shallow structure <strong>of</strong> the lower<br />

trench slope <strong>of</strong>f Nias Island, <strong>Sunda</strong> Arc. In: D.E. Hayes (ed.) The tectonic and geologic evolution <strong>of</strong> Southeast<br />

Asian seas and islands-1, AGU Geoph. Mon. 23, p. 179-208.<br />

<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 50 www.vangorselslist.com July 2012

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