Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Richmond, W.C., H. Dwidjojuwono, A. Tastari & B. Toha (2002)- Reservoir compartmentalization: an
integrated evaluation of supermature Minas oil field, Central Sumatra. Proc. 28th Ann. Conv. Indon. Petrol.
Assoc. 2, p. 137-156.
(Minas oil field produced more than four billion barrels of oil since early 1950’s. NW-SE trending anticline.
Main producing reservoirs, originally thought to be regionally continuous fluvial/deltaic sands, are commonly
compartmentalized, primarily due to complex stratigraphic and structural setting, with some post-depositional
diagenetic processes. Detailed depositional framework constructed using 1430 wells. Sequence stratigraphic
framework of E Miocene Bekasap Fm reservoir 11 regionally correlatable flooding surfaces and five sequence
boundaries in overall regressive-transgressive package)
Robinson, K.M. & A. Kamal (1988)- Hydrocarbon generation, migration and entrapment in the Kampar Block,
Central Sumatra. Proc. 17 th Ann. Conv. Indon. Petrol. Assoc., p. 211-256.
(Kampar Block 3 oil types. Majority of oils in fields along Merbau and Lirik Trends plus Pekan and Binio
Fields, sourced from deep lacustrine, non-marine algal Kelesa shales. Panduk and N Merbau probably sourced
from lake edge, mainly terrestrial/minor algal Kelesa shales. Parum Field probably sourced from Kelesa or,
Lakat coals and coaly shales. Generation of oils over narrow maturity range of Ro = 0.55- 0.64%. Lacustrine
Kelesa shale source rock in deepest parts of S Bengkalis half graben. Lateral extent mapped by
palaeogeography of pre-29 mybp sequence. Source rock mature and in main to late phase of oil generation.
Onset of major oil generation in Plio-Pleistocene, probably due to increase in heat flow. Distribution of oil
fields fault controlled. Migration distance small (2-10 km). Quantification of oil charge to prospects/Fields
along Lirik and Merbau Trends indicate Kelesa source can easily account for oil found in Block to date)
Rock, N.M.S., D.T. Aldiss, J.A. Aspden, M.C.G. Clarke, A. Djunuddin et al. (1983)- The geology of the
Lubuksikaping Quadrangle, Sumatra (Quadrangle 0716) 1:250,000. Geol. Res. Dev. Centre, Bandung, 60p.
Rock, N.M.S., H.H. Syah, A.E. Davis, D. Hutchison M.T. Styles & R. Lena (1982)- Permian to Recent
volcanism in northern Sumatra, Indonesia: a preliminary study of its distribution, chemistry and peculiarities.
Bull. Volcanologique 45, 2, p. 127-152.
(Sumatra has been volcanic arc above NE-dipping subduction zone since Late Permian. Main volcanic episodes
N of Equator: Late Permian, Late Mesozoic, Paleogene, Miocene and Quaternary. Late Permian volcanic rocks
are altered porphyritic basic lavas interstratified with limestones and phyllites. Late Mesozoic volcanic rocks
widely distributed along and W of Sumatra Fault System, include ophiolite-related spilites, andesites and
basalts. Miocene volcanic rocks widely distributed along W coast. Quaternary volcanism is irregular and
anomalous in relation to S Sumatra and adjacent Java-Bali)
Rodriguez, N.D. & R.P. Philp (2012)- Productivity and paleoclimatic controls on source rock character in the
Aman Trough, north central Sumatra, Indonesia. Organic Geochem. 45, p. 18-28.
(C Sumatra Basin oil sourced from Brown Shale Fm of Pematang Gp.. Oils in Aman Trough, variable
molecular and isotopic compositions, reflecting lateral facies variations in source rock. Source rock deposited
in fresh to brackish water stratified lake with CO2 limiting conditions. Isotopic data indicate changes in
paleoclimatic conditions, possibly associated with Eocene-Oligocene paleoclimatic transition)
Roemer, F. (1880)- Uber eine Kohlenkalk-fauna der Westkuste von Sumatra. Palaeontographica 27, p. 1-11.
('On a 'coal-limestone' (=Carboniferous) fauna from the West coast of Sumatra'. Same as Roemer 1981, below)
Roemer, F. (1881)- Uber eine Kohlenkalk-fauna der Westkuste von Sumatra. Jaarboek Mijnwezen Nederl.
Oost-Indie 10 (1881), 1, p. 289-305.
('On a 'coal-limestone' (=Carboniferous) fauna from the West coast of Sumatra'. First description of dark grey,
limestone from near Padang, W Sumatra, with striking resemblance to Upper Carboniferous ‘Kohlenkalk’ of
NW Europe. Contains fusulinids, brachiopods (incl. Productus sumatrensis n.sp.), crinoids, nautiloids,
gastropods and a trilobite (incl. Phillipsia sumatrensis n.sp.))
Roezin, S. (1974)- The discovery and development of Petapahan Oil Field, Central Sumatra. Proc. 3 rd Ann.
Conv. Indon. Petrol. Assoc., 1, p. 111-127.
Bibliography of Indonesia Geology v. 4.1 83 www.vangorselslist.com July 2012