Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Karig, D.E., S. Suparka, G.F. Moore & P.E. Hehunassa (1978)- Structure and Cenozoic evolution of the Sunda
Arc in the Central Sumatra region. CCOP Techn. Bull. 12, p. 43-86.
(Same paper as above)
Karig, D.E., S. Suparka, G.F. Moore & P.E. Hehunassa (1978)- Structure and Cenozoic evolution of the Sunda
Arc in the Central Sumatra region. In: Geological and geophysical investigations of continental margins, Am.
Assoc. Petr. Geol., Mem. 29, p. 223-237.
(W Sumatra margin reflects effects of subduction and right-lateral slip. Nias consists of mid-Tertiary melange
and less deformed younger beds. Forearc basin at least 4km sediment. Unconformity around Paleogene-
Miocene boundary. Inner shelf and coastal mountains common Oligocene andesitic intrusives and volcanics
(farther W than younger and older volcanic centers). Major uplift of Barisan Mts in Late Miocene- Pliocene)
Karig, D.E., S. Suparka, G.F. Moore & P.E. Hehunassa (1978)- Structure and Cenozoic evolution of the Sunda
Arc in the Central Sumatra region. UN ESCAP, CCOP Techn. Bull. 12, p. 87-108.
(Same paper as above)
Karta, K., Zuki & Isnawati (1998)- Geodynamics of the north Sumatra fore arc as caused by oblique
subduction: results of the Sumenta expedition of R.V. Baruna Jaya III. In: J.L. Rau (ed.) Proc. 34th Sess. Sess.
Co-ord. Comm. Coastal Offshore Geosc. Programs E and SE Asia (CCOP), Taejon, Korea 1997, 2, Techn.
Repts, p. 172-185.
Kastowo & G.W. Leo (1973)- Geologic map of the Padang Quadrangle, Sumatra (4/VIII), 1:250,000. Geol.
Res. Dev. Centre, Bandung.
Katili, J.A. (1960)- Geological investigations in the Lassi granite mass (Central Sumatra). Doct. Thesis Inst.
Techn. Bandung, 127p. (Unpublished)
Katili, J.A. (1962)- On the age of the granitic rocks in relation to the structural features of Sumatra. In: G.A.
MacDonald & H. Kuno (eds.) The crust of the Pacific Basin. Am. Geoph. Union Mon. 6, p. 116-121.
Most granites of Sumatra post-Triassic and pre-Tertiary in age, but some granites in S Sumatra of Cretaceous
age. In C Sumatra only one definite unconformity between Triassic and Tertiary deposits. No accurate age of
folding can be established from field data. Radiometric age of Lassi granites in C Sumatra 112 ± 24 Ma, mid-
Cretaceous= tied to folding?)
Katili, J.A. (1968)- Permian volcanism and its relation to the tectonic development of Sumatra. Bull. Nat. Inst.
Geol. Mining Bandung 1, 1, p. 3-13. (also in “ Geotectonics of Indonesia- a modern view’, Bandung 1980)
(Extensive Permian volcanics SE of Lake Singkarak, mainly flows of hornblende and augite andesites ('diabase
of Verbeek 1883). Thin-bedded limestone-shale in tuffs with Upper Permian fusulinids Doliolina lepida,
Pseudofusulina padangensis, Neoschwagerina multiseptata and Fusulinella lantenoisi. Local contact
metamorphism around mid-Cretaceous Lassi granites, simultaneous with main folding phase of region)
Katili, J.A. (1969)- Permian volcanism and its relation to the tectonic development of Sumatra. Bull.
Volcanologique 33, p. 530-540.
(same paper as above)
Katili, J.A. (1970)- Large transcurrent faults in Southeast Asia, with special reference to Indonesia. Geol.
Rundschau 59, 2, p. 581-600.
Katili, J.A. (1970)- Naplet structures and transcurrent faults in Sumatra. Bull. Nat. Inst. Geol. Mining, Bandung,
3, 1, p. 11-28.
(Disputes nappe structure of Sumatra Pre-Tertiary, as proposed by Tobler 1917)
Katili, J.A. (1973)- Geochronology of West Indonesia and its implication on plate tectonics. Tectonophysics 19,
p. 195-212.
Bibliography of Indonesia Geology v. 4.1 51 www.vangorselslist.com July 2012