Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
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trench slope break defines landward termination <strong>of</strong> accretionary prism. Velocities <strong>of</strong> outer high moderate,<br />
suggest sediments. Reduced reflectivity beneath rugged top basement supports high degree <strong>of</strong> deformation and<br />
compaction. Several km <strong>of</strong> sediment in forearc, with distinct basin recognized <strong>of</strong>f S <strong>Sumatra</strong> but not <strong>of</strong>f <strong>Sunda</strong><br />
Strait. Bathymetric elevation <strong>of</strong> Java shelf in S <strong>Sunda</strong> Strait corresponds to increased basement high velocities<br />
and is connected to <strong>Sunda</strong> Strait transtensional basin. Velocity-depth model indicates continental-type crust<br />
under forearc basin <strong>of</strong>f S <strong>Sumatra</strong>, whereas lower velocities found beneath <strong>Sunda</strong> Strait forearc)<br />
Kopp, H., R. Weinrebe, S. Ladage, U. Barckhausen, D. Klaeschen, E.R. Flueh, C. Gaedicke, Y. Djajadihardja et<br />
al. (2008)- Lower slope morphology <strong>of</strong> the <strong>Sumatra</strong> trench system. Basin Research 20, p. 519-529.<br />
(Lower plate fabric extensively modulates upper plate morphology and morphotectonic segmentation <strong>of</strong><br />
<strong>Sumatra</strong> trench system is linked to subduction <strong>of</strong> reactivated fracture zones and aseismic ridges <strong>of</strong> Wharton<br />
Basin. In general, increasing intensity <strong>of</strong> mass-wasting processes, from S to N, correlates with oversteepening<br />
<strong>of</strong> lower slope, probably in response to alternating phases <strong>of</strong> frontal accretion and sediment underthrusting)<br />
Koulakov, I., T. Yudistira, B.G. Luhr & Wandono (2009)- P, S velocity and VP/VS ratio beneath the Toba<br />
caldera complex (Northern <strong>Sumatra</strong>) from local earthquake tomography. Geoph. J. Int. 177, 3, p. 1121-1139.<br />
Krausel, R. (1922)- Fossile Holzer aus dem Tertiar von Sud-<strong>Sumatra</strong>. Beitr. Geol. Palaont. <strong>Sumatra</strong> 4, Verhand.<br />
Geol. Mijnbouwk. Gen. Nederl. Kol., Geol. Ser. 5, 5, p. 231-287.<br />
('Fossil wood from the Tertiary <strong>of</strong> South <strong>Sumatra</strong>'. Descriptions <strong>of</strong> Miocene silicified woods collected by<br />
Tobler. Up to 10m long silicified tree trunks in tuffaceous Upper Miocene Lower Palembang Fm. Some name<br />
changes suggested by Den Berger (1923))<br />
Krausel, R. (1929)- Fossile Pflanzen aus dem Tertiar von Sud-<strong>Sumatra</strong>. Beitr. Geol. Pal. <strong>Sumatra</strong> 11, Verhand.<br />
Geol. Mijnbouwk. Gen. Nederl. Kol., Geol. Ser. 9, 1, p. 1-44.<br />
('Fossil plants from the Tertiary <strong>of</strong> South <strong>Sumatra</strong>'. Description <strong>of</strong> plants collected by Tobler from M and U<br />
Palembang Fms. Late Miocene S <strong>Sumatra</strong> forests not much different from present-day. No locality maps,<br />
stratigraphy)<br />
Kristanto, A.S. (1991)- Structural analysis <strong>of</strong> the <strong>Sumatra</strong>n Fault Zone around the Semangka Bay. Proc. 20th<br />
Ann. Conv. Indon. Assoc. Geol. (IAGI), p. 354-375.<br />
Krumbeck, L. (1914)- Obere Trias von <strong>Sumatra</strong> (Die Padang-Schichten von West-<strong>Sumatra</strong> nebst Anhang).<br />
Palaeontographica Suppl. IV, Beitr. Geologie Niederländisch-Indien II, 3, p. 195-266.<br />
(Stratigraphy- paleontology <strong>of</strong> ~200m thick Upper Triassic Padang beds. Poorly fossiliferous sandstones,<br />
shales and marls, but four layers <strong>of</strong> blue-grey, marly fossiliferous, platy limestones. Bivalve faunas look related<br />
to Carnian North-Apine Cardita facies. Absence <strong>of</strong> Misolia, despite same age as Fogi Beds <strong>of</strong> Buru?)<br />
Kugler, H. (1921)- Geologie des Sangir-Batangharigebietes (Mittel-<strong>Sumatra</strong>). Verhand. Geol. Mijnbouwk. Gen.<br />
Nederl. Kol., Geol. Ser. 5, 4, p. 135-201.<br />
(<strong>Geology</strong> <strong>of</strong> the Sangir- Batang Hari area', S part <strong>of</strong> Padang Highlands, N <strong>of</strong> Korinci volcano. Metamorphic<br />
rocks <strong>of</strong> ‘Schieferbarisan’, Permian fusulinid limestones, Late Triassic limestones with Cardita and with<br />
Gervilia and Loxonema molluscs, granites, peridotites, etc.)<br />
Kurnely, K., B. Tamtono, S. Aprilian & I. Doria (2003)- A preliminary study <strong>of</strong> development <strong>of</strong> Coalbed<br />
Methane (CBM) in South <strong>Sumatra</strong>. SPE Asia Pacific Oil and Gas Conf., Jakarta 2003, 6p.<br />
(South <strong>Sumatra</strong> onshore basin assesed potential Coal Bed Methane gas 120 TCF. Not much detail)<br />
Kurnio, H., U. Schwarz-Schampera & M. Wiedicke (2008)- Structural geological control on the mineralization<br />
on Tabuan Island, Semngko Bay, South Sumatera, <strong>Indonesia</strong>. Bull. Marine Geol. 23, 1, p. 18-25.<br />
(online at: http://isjd.lipi.go.id/admin/jurnal/231081825.pdf)<br />
(Basaltic-andesitic volcanics <strong>of</strong> Late Oligocene- earliest Miocene Hulusimpang Fm distributed in broad zone<br />
along Semangko Fault zone and are hosts for several epithermal-style gold deposits. Mineralization on Tabuan<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 56 www.vangorselslist.com July 2012
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