Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

(Cenozoic stratigraphy of N and E parts of N Sumatra well established, from oil and gas exploration activities.
Modified formation names proposed. Depositional model postulates presence off NW of Sumatra, of a chain of
non-volcanic outer arc islands between 35/32 Ma - 18/17 Ma, similar to present Nias-Mentawai islands. E-M
Miocene uplift of Asahan Arch and volcanism, mid-Miocene orogeny linked to initial opening of Andaman Sea,
Late Miocene- Quaternary volcanism, and latest Plio-Pleistocene orogenic pulse)
Keil, K.F.G. (1931)- Over het ontstaan van karakteristieke kalk concreties in de Telisa-lagen aan den oostrand
van het Goemai-gebergte. De Mijningenieur 12, p. 193-198.
('On the origin of characteristic calcareous concretions in the Telisa beds at the E margin of the Gumai
Mountains'. Formed by physical- chemical processes)
Kelley, P.A., B. Mertani & H.H. Williams (1995)- Brown Shale Formation: Paleogene lacustrine source rocks
of Central Sumatra. In: B.J. Katz (ed.) Petroleum source rocks, Springer-Verlag, Berlin, p. 283-308.
Kertapati, E.K. (1984)- Penelitian seismotektonik Teluk Lampung dan sekitarnya. Proc. 13th Ann. Conv. Indon.
Assoc. Geol. (IAGI), p. 65-96.
('Investigation of seismotectonics of Lampung Bay and surroundings')
Kesumajana, A.H.P., D. Noeradi, B. Sapiie & A. Priono (2010)- The role of hydrocarbon maturation modeling,
A case study: South Sumatra Basin. Proc. 34th Ann. Conv. Indon. Petrol. Assoc., IPA10-G-147, 4 p.
(Summary of thermal modeling study in S Sumatra basin from hydrocarbon maturity data. Five phases: (1)
increase in heat flow during rift phase (30.5- 25 Ma), (2) decrease during sag phase (25- 20 Ma), (3) increase
again due to magmatic activity (20- 10 Ma), (4) decline after cessation of magmatism (10- 1.6 Ma) and (5)final
increase with final magmatic activity (1.6- 0 Ma).
Khan, P.K. & P.P. Chakraborty (2009)- Bearing of plate geometry and rheology on shallow-focus mega-thrust
seismicity with special reference to 26 December 2004 Sumatra event. J. Asian Earth Sci. 34, p. 480-491.
Kieckhefer, R.M., G.F. Moore, F.J. Emmel & W. Sugiarta (1981)- Crustal structure of the Sunda forearc region
west of central Sumatra from gravity data. J. Geophys. Res. 86, p. 7003-7012.
(Gravity modeling of transect S of Nias. Free-air anomalies -100 mGal low 10-20 km landward of trench axis
and +80 mGal high over outer arc ridge but also large anomalies unrelated to topography. An 80 mGal rise
may be near-surface body of high-density material (oceanic crust?). This slab may be exposed on SW coast of
Nias, where ultramafic bodies were mapped. A -30 mGal free-air low over forearc basin modeled best if pre-
Miocene mélange or continental crust underlies basin)
Kieckhefer, R.M., G.G. Shor, J.R. Curray, W. Sugiarta & F. Hehuwat (1980)- Seismic refraction studies of the
Sunda trench and forearc basin. J. Geophys. Res. 85, B2, p. 863-889.
(Six refraction lines around Nias Island, NW Sumatra, parallel to structure)
Kieft, C. & I.S. Oen (1973)- Ore minerals in the Telluride-bearing gold-silver ores of Salida, Indonesia, with
special referenc to the distribution of Selenium. Mineral. Deposita 8, p. 312-320.
Kieft, C. & I.S. Oen (1977)- Ore mineral parageneses in Mn-Sn-Ag-Au-Se-bearing veins of Mangani, Sumatra,
Indonesia. In: Problems of ore deposition 2, 4 th IAGOD Symposium, Varna, Publ. House Bulgarian Acad. Sci.,
Sofia, p. 295-302.
Kimpe, W.F.M. (1944)- De eruptiva van het Siboemboen-gebergte en hun contactgesteenten (Padangsche
Bovenlanden, Sumatra). Doct. Thesis University. of Amsterdam, 141p.
(Descriptions of igneous rocks of Sibumbum Mountains, E of Lake Singkarak, Padang Highlands)
Kingston, J. (1978)- Oil and gas generation, migration and accumulation in the North Sumatra Basin. Proc. 7th
Ann. Conv. Indon. Petrol. Assoc., Jakarta, p. 75-104.
Bibliography of Indonesia Geology v. 4.1 53 www.vangorselslist.com July 2012