Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

(Acoustic surveys and core holes between Singkep and Bangka and around Karimata islands. Basement
covered by unconsolidated sub-horizontal sands with peat interbeds, probably Late Tertiary age. Followed by
sediment-filled gullies, incised into older sediments, also with peat, also Late Tertiary. Near-horizontal
planation surface at 20-30m below sea level, overlain by young marine sediments)
Archbold, N.W. (1983)- A Permian nautiloid from Belitung, Indonesia. Publ. Geol. Res. Dev. Center, Bandung,
Paleont. Ser. 4, p. 32-36.
(Fragment of nautiloid Neorthoceras suggests E Permian age for part of NE Belitung Island 'basement' rocks.
With summary of other Late Paleozoic macrofossil occurrences)
Aryanto, N.C.D., N. Sukmana & P. Rahardjo (2001)- Specific heavy minerals study on the South Bangka
island: a statistical approach. In: Proc. CCOP 37th Ann. Sess. Bangkok 2000, 2, Techn. Repts., p. 65-70.
Baartmans, J.A., H. Boissevain, J. van Galen, P.H. Kuenen, T. Raven, G.L. Smit Sibinga, J. Weeda & J.I.S.
Zonneveld (1947)- De morfologie van de Java- en Soenda Zee. Tijdschr. Kon. Ned. Aardr. Gen. II-64, p. 442-
465 and p. 555-576.
('The morphology of the Java and Sunda Sea'. Overview of Java Sea morphology and morphological history)
Baharuddin & Sidarto (1995)- Geologic map Belitung, Sumatra. Geol. Res. Dev. Centre, Bandung.
Batchelor, B.C. (1979)- Geological characteristics of certain coastal and offshore placers as essential guides for
tin exploration in Sundaland, Southeast Asia. Bull. Geol. Soc. Malaysia 11, p. 283-313.
(Over 95% of tin production in Malaysia and Indonesia from 'alluvial' placers. Discontinuously rising late
Cenozoic eustatic sea-levels and accompanying climate changes main controls on Sundaland sedimentation.
Late Cenozoic subdivided into Sundaland regiolith (Late Miocene- E Pliocene), Older sedimentary cover
(Pliocene- E Pleistocene) and Young Alluvium (Late Pleistocene- Holocene))
Batchelor, B.C. (1979)- Discontinuously rising late Cainozoic eustatic sea-levels, with special reference to
Sundaland, Southeast Asia. Geologie Mijnbouw 58, 1, p. 1-20.
(M Miocene- Recent cyclicity)
Bellwood, P. (1990)- From Late Pleistocene to Early Holocene in Sundaland. In: C. Gamble & O. Soffer (eds.)
The world at 18 000 BP; II, Low latitudes, p. 255-263.
Ben-Avraham, Z. & K.O. Emery (1973)- Structural framework of Sunda Shelf. Am. Assoc. Petrol. Geol. Bull.
57, p. 2323-2366.
Bird, M. I., W.C. Pang & K. Lambeck (2006)- The age and origin of the Straits of Singapore. Palaeogeogr.
Palaeoclimatol. Palaeoecol. 241, p. 531-538.
Bodenhausen, J.W.A. (1954)- The mineral assemblage of some residual monazite- and xenotime-rich cassiterite
deposits of Banka (Indonesia). Proc. Kon. Nederl. Akad. Wet. B57, 3, p. 322-328.
(Heavy minerals of young clastics of Muntok District, Bangka, 30-60% cassiterite, 19-22% monazite, 11-31%
ilmenite, 1-5% xenotime)
Bon E.H. (1979)- Exploration techniques employed at the Pulau Tujuh tin discovery. In: A. Prijono, C. Long
and R. Sweatman (eds.) The Indonesian mining industry, its present and future, Proc. First Indonesian Mining
Symposium, Jakarta 1977, Indon. Mining Assoc., Jakarta, p 147-183.
Bothe, A.C. (1924)- Enkele opmerkingen over stroomtinertsvorming op het eiland Bintan. De Mijningenieur 5,
9, p. 146-151.
('Some remarks of the formation of alluvial tin ore on Bintan island'. With geologic map S Bintan 1:150,000)
Bibliography of Indonesia Geology v. 4.1 127 www.vangorselslist.com July 2012