Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Nur'aini, S., S. Martodjojo, F.W. Musgrove & J. Bon (2001)- Revisiting the Middle Baong sand: basin floor fan
or slope fan in origin? Berita Sediment. 15, p. 6-9.
Nuryadin, H., F. Kamil, A. Kamal & R.M.I. Argakoesoemah (2006)- A challenge and future potential of basal
clastic play in Paleo-Basement High, Musi Platform, South Sumatra Basin. Proc. Jakarta 2006 Int. Geosc. Conf.
Exhib., Indon. Petrol. Assoc., Jakarta06-PG-23, p. 1-5.
(Musi Platform traditional objective is Baturaja carbonates. Most exploration wells drilled basement, some
have thin Basal Clastics unit, possibly equivalent to Upper Talang Akar Fm. Hydrocarbon potential of basal
clastic play shown by successful tests in recent wells like Soka F-2, Kembar-1, and Fariz-3. Reservoir quality
variable. Play mostly a combination stratigraphy- structure)
Oostingh, C.H. (1941)- Over de Tertiaire molluskenfauna van Palembang. De Ingen. Nederl. Indie 8, p. 21-29.
(‘On the Tertiary mollusc fauna from Palembang’)
Oppenoorth, W.F. (1918)- Foraminiferen van de Noordkust van Atjeh. Verhand Geol-Mijnbouwk. Gen., Geol.
ser. 2, p. 249-258.
(‘Foraminifera from the North coast of Aceh’. At several localities limestone at base of Neogene, rich in
Lepidocyclina Miogypsina, Cycloclypeus. Interbedded with marls with Orbulina universa. Age assumed to be
Aquitanian, but more likely Middle Miocene; HvG)
Oppenoorth, W.F.F. & J. Zwierzycki (1918)- Geomorfologische en tektonische waarnemingen als bijdrage tot
verklaring van de landschapsvormen van Noord Sumatra. Jaarboek Mijnwezen Nederl. Oost-Indie 46 (1917),
Verhand. I, p. 276-311.
(‘Geomorphological and tectonic observations as a contribution to the explanation of the landforms of North
Sumatra’)
Osberger, R. (1954)- Die Geologie des Sibumbungebirges nebst Beschreibung der hier und in benachbarten
Gebieten liegenden Ertzvorkommen (Mittel-Sumatra). Sitzungsber. Osterr. Akad.Wiss., Math.-Naturw. Kl., 1,
163, 9-10, p. 689-723.
('The geology of the Sibumbun Mountrains with description of the associated and nearby ore occurrences (C
Sumatra)'. Summary of geology and copper and iron mineralizations associated with Carboniferous- Triassic
intrusives in NE of Singkarak Lake, Padang province)
Osberger, R. (1955)- Uber Deckenbau und andere geologische Probleme im Pratertiair Sumatras. Neues Jahrb.
Geol. Palaont., Monarshefte 1955, 8, p. 321-341.
(‘On nappe structures and other geological problems in the Pre-Tertiary of Sumatra’. Assumes existence of
nappe structure in Toba area of N Sumatra)
Osberger, R. (1956)- On the nappe structure and other geological problems in the Pre-Tertiary of Sumatra. 20 th
Sess. Int. Geol. Congr., Mexico, 5, p. 411-420.
(Assumes existence of nappe structure in Toba area of N Sumatra)
Ozawa, Y. (1929)- A new occurrence of Schwagerina princeps in Sumatra. Eclogae Geol. Helv. 22, p. 51-52.
(Occurrence of fusulinids in Productus limestone of Teluk Gedang on Merangin River, below plant beds with
Pecopteris of Garing River)
Page, B.N.G., J.D. Bennett, N.R. Cameron, D.M. Bridge, D.H. Jeffrey et al. (1979)- A review of the main
structural and magmatic features of northern Sumatra. J. Geol. Soc., London, 136, 5, p. 569-579.
(Three main periods of Cenozoic volcanismin N Sumatra: E Oligocene, Oligo-Miocene and Miocene- Recent.
Large transcurrent movements on SFS indicated by (a) regional slivers of oceanic crust trapped at leading
junction of W continental plate as it moved NW against main mass of island; (b) palaeomagnetic evidence
showing E Sumatra as part of Malaya block and in equatorial position since Cretaceous, while palaeolatitude
of NW tip of Sumatra (W of SFS), was farther S; (c) juxtaposition of Li-rich and Li-poor geochemical provinces
Bibliography of Indonesia Geology v. 4.1 75 www.vangorselslist.com July 2012