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Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

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McCarthy, A.J. (1997)- The evolution <strong>of</strong> the transcurrent <strong>Sumatra</strong>n fault system, <strong>Indonesia</strong>. Ph.D. Thesis,<br />

University London, 387 p.<br />

McCarthy, A.J. & C.F. Elders (1997)- Cenozoic deformation in <strong>Sumatra</strong>: oblique subduction and the<br />

development <strong>of</strong> the <strong>Sumatra</strong>n fault system. In: A.J. Fraser & S.J. Matthews (eds.) Petroleum <strong>Geology</strong> <strong>of</strong> SE<br />

Asia. Geol. Soc., London, Spec. Publ. 126, p. 355-363.<br />

(<strong>Sumatra</strong> pre-Tertiary history <strong>of</strong> accretion was followed byPalaeogene basin formation. Strong mid-Miocene<br />

inversion event recorded in onshore part <strong>of</strong> forearc basin in S <strong>Sumatra</strong>, same time as inception <strong>of</strong> seafloor<br />

spreading in Andaman Sea and probable inception <strong>of</strong> major strike-slip movement along the SFS, possibly<br />

following clockwise rotation <strong>of</strong> <strong>Sumatra</strong> towards it present NW-SE trend. SFS complex deformation history<br />

including polyphase reactivation <strong>of</strong> fault surfaces and contemporaneous strike-slip and orthogonal compression<br />

or extension. New estimate <strong>of</strong> ~150 km <strong>of</strong>fset <strong>of</strong> Mesozoic units across SFS in C <strong>Sumatra</strong> proposed. Several<br />

basins formed along SFS in Quaternary)<br />

McCarthy, A.J., B. Jasin & N.S. Haile (2001)- Middle Jurassic radiolarian chert, Indarung, Padang District, and<br />

its implications for the tectonic evolution <strong>of</strong> western <strong>Sumatra</strong>, <strong>Indonesia</strong>. J Asian Earth Sci. 19, 1-2, p. 31-44.<br />

(Radiolaria chert in Indarung Area, E <strong>of</strong> Padang, Aalenian (lower M Jurassic) age. Carbonate in area dated as<br />

U Jurassic- E Cretaceous based occurrence <strong>of</strong> Lovcenipora (more likely Late Triassic?; HvG), and overlying<br />

tuff K/Ar age <strong>of</strong> ~105 Ma/ Albian, but suspect. Chert probably faulted into younger limestone during ENEdirected<br />

compression. This is one <strong>of</strong> best dated occurrences <strong>of</strong> allochthonous material in <strong>Sumatra</strong> and confirms<br />

accretion <strong>of</strong> oceanic material along <strong>Sunda</strong> margin in M- Late Cretaceous)<br />

McCloskey, J., D. Lange, F. Tilmann, S.S. Nalbant, A.F. Bell, D.H. Natawidjaja & A. Rietbrock (2010)- The<br />

September 2009 Padang earthquake. Nature Geoscience, doi:10.1038/ngeo753, p.<br />

McCourt, W.J. & E.J. Cobbing (1993)- The geochemistry, geochronology and tectonic setting <strong>of</strong> granitoid rocks<br />

from southern <strong>Sumatra</strong>, western <strong>Indonesia</strong>. S. <strong>Sumatra</strong> Geol. Mineral Exploration Project Report Ser. 9, Geol.<br />

Res. Dev. Centre, Bandung, p.<br />

McCourt, W.J., M.J. Crow, E.J. Cobbing & T.C. Amin (1996)- Mesozoic and Cenozoic plutonic evolution <strong>of</strong><br />

SE Asia: evidence from <strong>Sumatra</strong>, <strong>Indonesia</strong>. In: R. Hall & D. Blundell (eds.) Tectonic evolution <strong>of</strong> Southeast<br />

Asia, Geol. Soc. Spec. Publ. 106, p. 321-335.<br />

(Barisan Mts <strong>of</strong> S <strong>Sumatra</strong> four periods <strong>of</strong> plutonic activity: Miocene-Pliocene (20-5 Ma), E Eocene (60-50<br />

Ma), Mid-Late Cretaceous (117-80 Ma) and Jurassic-E Cretaceous (203-130 Ma). Also plutonic activity in<br />

Permian (287-256 Ma) and suggestions <strong>of</strong> magmatism in Late Triassic- E Jurassic (220-190 Ma) and M<br />

Jurassic-E Cretaceous (170-130 Ma). Ages from E <strong>Sumatra</strong> indicate Triassic- E Jurassic (240-195 Ma) tin-belt<br />

magmatism <strong>of</strong> Peninsular Malaysia Main Range extends into area. Plutonic suites in NW-SE trending belts.<br />

Breaks in plutonic activity correspond to changes in approach angle and/or rate <strong>of</strong> subduction, and in some<br />

instances relate to periods <strong>of</strong> collision and accretion <strong>of</strong> allochthonous material. At least two such events: early<br />

M Cretaceous collision and accretion <strong>of</strong> oceanic Woyla terranes, and latest Cretaceous possible collision <strong>of</strong><br />

continental sliver/block, the W <strong>Sumatra</strong> terrane to <strong>Sunda</strong>land margin)<br />

Meckel, L., M. Gidding, M. Banukarso, D. Sim, A. Setoputri, A. Abimanyu, M. Sompie, N. Citajaya & M.<br />

Gunarto (2012)- Hydrocarbon systems <strong>of</strong> the <strong>of</strong>fshore North <strong>Sumatra</strong> Basin, <strong>Indonesia</strong>. Proc. 36th Ann. Conv.<br />

Indon. Petrol. Assoc., IPA12-G-012, p. 1-11.<br />

(Offshore North <strong>Sumatra</strong> Basin considered under-explored, with 130 <strong>of</strong>fshore exploration wells drilled through<br />

2011. At least 5 plays, syn-rift Oligocene clastics (Parapat Fmn), Oligocene-Miocene carbonate build-ups<br />

(Tampur and Peutu Fms), and Miocene-Pliocene turbidites (Bampo, Baong, Keutapang, and Seurula Fms))<br />

Mertani, B. et al. (1996)- Petroleum geology <strong>of</strong> the Central <strong>Sumatra</strong> basins. In: Pertamina BPPKA Petroleum<br />

geology <strong>of</strong> <strong>Indonesia</strong>, II, p. 157-192.<br />

Mertosono, S. (1975)- <strong>Geology</strong> <strong>of</strong> Pungut and Tandun oil fields, Central <strong>Sumatra</strong> Basin. Proc. 5 th Ann. Conv.<br />

Indon. Petrol. Assoc., p. 156-179.<br />

<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 65 www.vangorselslist.com July 2012

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