Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Houtz, R.E. & D.E. Hayes (1984)- Seismic refraction data from Sunda Shelf. Am. Assoc. Petrol. Geol. Bull. 68,
12, p. 1870-1878.
(Seismic refraction data along 2 Sundaland profiles, one NW of Natuna island, one off N Borneo. Offshore
Sarawak Basin underlain by oceanic crust and now covered by 8 km of undisturbed sediment, implying that
shelf edge has advanced about 300 km N-ward over oceanic crust as result of post-Eocene progradation)
Hovig, P. (1920)- Banka, the geology and the tin ores. Gen. Engin. Congr., Batavia May 1920, 41 p.
Huguenin, J.A. (1877)- Rapport van het district Toboali, eiland Bangka. Jaarboek Mijnwezen Nederl. Oost-
Indie 6 (1877), 1, p. 81-185.
(Early geological- mining survey of Bangka island. With rel. detailed 1:60,000 scale geologic map)
Hutchison, C.S. (1968)- Invalidity of the Biliton granite, Indonesia, for determining the Jurassic/ Upper Triassic
boundary in the Thai-Malayan orogen. Geol. Mijnbouw 47, 1, p. 56-60.
Isaacs, K.N (1963)- Interpretation of geophysical profiles between Singapore and Labuan, North Borneo.
Geophysics 28, 5, p. 805-811.
(Airborne magnetometer profile and gravity profile from Singapore to Labuan, N Borneo, indicates shallow
basement along W half of profile, except for minor sedimentary basins ~50 miles W of Tambelan Islands and in
W Borneo. East of Kuching, Sarawak, major basin, with ~10,000’ sediment)
Johnson, H.D., F.A. Alqahtani, C.A.L. Jackson, M.R.B. Som, D.P. Ghosh & W.K.W. Sulaiman (2010)- Fluvial
reservoir analogues in the Malay Basin: analysis of shallow 3D seismic data of Pleistocene rivers on the Sunda
Shelf. In: L.J. Wood et al. (eds.) Seismic imaging of depositional and geomorphic systems, Gulf Coast Sect.
SEPM, Ann. Perkins Research Conf. 30, Houston, p. 328-329.
Johnson, R.F. & Marjono (1963)- Geology and bauxite deposits of the central Riau Islands, Indonesia.
Direktorat Geologi, Bandung, Publ. Teknik, Seri Geologi Ekonomi 6, p. 1-54.
(Occurrence of bauxite on several islands of Riau Archipelago (Lobam, Ngenang), in addition to known Bintan
occurrences. Some laterites residual on granitic rocks, some in marine terraces)
Jones, M.T., B.L. Reed, B.R. Doe & M.A. Lanphere (1977)- Age of tin mineralization and plumbotectonics,
Belitung, Indonesia. Econ. Geol. 72, p. 745-752.
(Primary tin deposits on Belitung related to Upper Triassic granites with Rb-Sr isochron age of 213 + - 5 Ma.
Average K-Ar age of muscovite from two cassiterite-bearing greisens 198 Ma, suggesting tin mineralization is
not simple late-stage event in emplacement of plutons)
Jongmans, W.J. (1951)- Fossil plants of the Island of Bintan. Proc. Kon. Nederl. Akad. Wetensch., B54, 2, p.
183-190.
(First description of latest Triassic 'Bintan flora', Riau islands. More comparable to Neocomian of W Malaysia
according to Kon’no (1972), but still considered to be Rhaetian-Liassic by Wade (2008))
Junker, H.W. (1936)- Bauxit und Laterit auf Banka. Ein Beitrag zur Kenntnis der Geologie von Banka. De
Ingen. in Nederl. Indie IV, 3, p. 15-23.
('Bauxite and laterite on Bangka; a contribution to the knowledge of the geology of Bangka')
Kanayama, S. (1973)- Tin bearing granites and tin placers in Bangka and Billition islands, in Indonesia. Kyoto
University, Southeast Asian Studies 11, 3, p. 321-337.
(Online at: http://kyoto-seas.org/pdf/11/3/110302.pdf kyoto-seas. Mainly in Japanese)
(Tin in Indonesia mainly exploited from placers with cassiterite. Source rocks are tin granites of collision type,
which are more common in Europe and USA than Cardilleran type of Japan. Economic cassiterite
concentrations limited to area within 14-15 km from edges of granitic mother rocks)
Bibliography of Indonesia Geology v. 4.1 132 www.vangorselslist.com July 2012