Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Van Overeem, A.J.A. (1960)- The geology of the cassiterite placers of Billiton, Indonesia. Geol. Mijnbouw 39,
10, p. 444-457.
(Probable Cathaysian Permian plant assemblages on Billiton and Cathaysian Permian schwagerinid fusulinids
in borehole off North Billiton)
Van Raadshoven, B. & J. Swart (1942)- On rocks from Karimon (Riouw Archipelago). Proc. Kon. Nederl.
Akad. Wetensch., Amsterdam, 45, 1, p. 89-96.
(online at: http://www.dwc.knaw.nl/DL/publications/PU00017704.pdf)
(Karimun island, SW of Singapore. Rocks collected by Roggeveen. Most of island post-Triassic biotite granites.
Sediments in NE of island contact-metamorphic slates, quartzites, limestone, etc., possibly of Carboniferous and
Triassic age. Basic plutonic rocks and associated metamorphics (metagabbros, diallagites, microfolded
hornblende schists identical to schists of Singkep lsland) on small islands Temblas and Merak, off S coast of
Karimun. Interpreted to be trace of Raub-Bentong Triassic suture zone by Pulunggono and Cameron 1984)
Van Wessem, A. (1941)- On rocks from the islands of Soegi, Tjombol and Tjitlim, Riouw Archipelago,
Netherlands East Indies. Proc. Kon. Nederl. Akad. Wetensch., Amsterdam, 44, 10, p. 1219-1226.
(online at: http://www.dwc.knaw.nl/DL/publications/PU00017686.pdf)
(Petrographic descriptions of rocks collected by Roggeveen: schists, radiolarian chert as pebbles in
conglomerate, quartzite, sandstones, greywackes, porphyrite, diotite, etc.) )
Verbeek, R.D.M. (1897)- Geologische beschrijving van Bangka en Billiton. Jaarboek Mijnwezen Nederl. Oost-
Indie 26, Verh., p. 1-272.
(Geological description of Bangka and Billiton (Belitung) Islands, E Sumatra, with focus on occurrences of tin)
Verbeek, R.D.M. (1897)- Glaskogels van Billiton. Jaarboek Mijnwezen Nederl. Oost-Indie, Wet. Ged., 1897, p.
235-272
('Glass pebbles from Billiton'. Early description of Pleistocene tektites, locally common on Belitung island (part
of large SE Asian- Australia tektite-strewn field, dated at ~0.7 Ma; see also Krause (1898), Wing Easton
(1915), Von Koenigswald (1935), Chapman (1964), etc.; HvG)
Von Koenigswald. G.H.R. (1933)- Soenda-plat en poolverplaatsing. De Mijningenieur. 14, p. 124-130.
(‘The Sunda Shelf and polar wandering’)
Wade-Murphy, J. & J.H.A. van Konijnenburg-van Cittert (2008)- A revision of the Late Triassic Bintan flora
from the Riau Archipelago (Indonesia). Scripta Geologica 136, p. 73-105.
(Online at: http://dpc.uba.uva.nl/08/nr136/a04) (Flora from SW Bintan Island, Riau Archipelago, partly
described by Jongmans in 1951. Additional taxa determined. Absence of fern and sphenophytes and dominance
of diminutive Pterophyllum and Ptilophyllum leaves. Stronger similarities between Bintan and SW Asian than
with SE Asian floras. Differences may point to slightly younger age (E-M Jurassic), but unlikely to be Early
Cretaceous as suggested by Kon’no 1972)
Wang, X.M., X.J. Sun, P.X. Wang & K. Stattegger (2007)- A high-resolution history of vegetation and climate
history on Sunda Shelf since the last glaciation. Science in China Ser., D- Earth Sci., 50, p. 75-80.
(16,500-year high-resolution pollen and spore records from sediments of core 18287 on continental slope of
southern S China Sea. Between 16.5-13.9 ka BP low-mountain rainforest dominated. In 13.9-10.2 ka BP
lowland rainforest and ferns expanded, indicating warming at last deglaciation and pollen sedimentation rates
reduced, implying rise of sea level/ sub-mergence of shelf. After 10.2 ka BP, decreasing fern indicates early
Holocene (10.2- ka B.P.) cold period, while increasing of fern marks rising temperature (7-3.6 ka BP).
Warburg, O. (1897)- Zwei neu fossile Phanerogamen-Gattungen von der Insel Bangka. Jaarboek Mijnwezen
Neder. Oost Indie 26, p. 229-234.
('Two new phanerogam species from Bangka island'. Pliocene plant fossils)
Bibliography of Indonesia Geology v. 4.1 140 www.vangorselslist.com July 2012