Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology

Katili, J.A. (1967)- Structure and age of the Indonesian tin belt with special reference to Bangka.
Tectonophysics 4, p. 403-418.
(Radiometric ages Billiton-Singkep granites Late Jurassic (too young?; HvG). Oldest rocks in Bangka
fossiliferous Permo-Carboniferous and Triassic; locally metamorphosed. Folding in Bangka probably also Late
Jurassic)
Katili, J.A. (1968)- Cross-folding in Bangka, West Indonesia. Contr. Dept. Geol. Inst. Tekn. Bandung 68, p. 61-
70.
(Cross-folds in N Bangka result of two orogenic movements.: NW-SE trending folds formed in Late Jurassic,
superimposed on NE-SW structures probably Paleozoic)
Keller, G.H. & A.F. Richards (1967)- Sediments of the Malacca Strait, Southeast Asia. J. Sedim. Petrology 37,
p. 102-127.
Kieft, C. (1952)- Accessory transparent minerals in tin granites of North Banka, Indonesia. Proc.Kon. Nederl.
Akad. Wetensch. B55, p. 140-149.
(Accessory heavy minerals in Banka tin granites include zircon, orthite, xenotime, monazite and allanite)
Kiel, B.A. & L.J. Wood (2010)- Correlations among seismic attributes and incised valley thicknesses in recent
stratigraphy of the Sunda Shelf, Indonesia. In: L.J. Wood, T.T. Simo & N.C. Rosen (eds.) Seismic imaging of
depositional and geomorphic systems, Gulf Coast Sect. SEPM, Ann. Perkins Research Conf. 30, Houston, p.
23-48.
Ko, U. Ko (1986)- Preliminary synthesis of the geology of Bangka Island, Indonesia. In: In: G.H. Teh & S.
Paramananthan (eds.) Proc. GEOSEA V Conf., Kuala Lumpur 1984, 2, Geol. Soc. Malaysia Bull. 20, p. 81-96.
(Stratigraphy Bangka 4 main units: (1) U Paleozoic Pemali Gp deep marine sediments, (2) M-U Triassic
marine Tempilang Sst, (3) Lw Tertiary Fan Fm fluvial deposits and (4) U Tertiary- Quaternary Ranggam Gp.
Thrusting and granitizaton and uplift in Late Triassic- E Cretaceous, followed by N-S high-angle cross faulting.
At Toboali in S Bangka, Permo-Carboniferous with glaciogenic ‘pebbly mudstones'?)
Koesoemadinata, R.P.K. & A. Pulunggono (1975)- Geology of the southern Sunda Shelf in reference to the
tectonic framework of Tertiary sedimentary basins of Western Indonesia. J. Indon. Assoc. Geol. (IAGI) 2, 2, p.
1-11.
Kruizinga, A. (1950)- Agathiceras sundaicum Han., a Lower Permian fossil from Timor (should be Billiton).
Proc. Kon. Akad. Wetensch. Amsterdam 53, 7, p. 1056-1063.
(online at: http://www.dwc.knaw.nl/DL/publications/PU00018850.pdf)
(First Paleozoic fossil found on Billiton island is small ammonite in lump of cassiterite from Lenggang district.
Identified as Agathiceras sundaicum, also common in Lower Permian of Timor (Bitauni). New find indicates
presence of Lower Permian sediments, subsequently intruded/ metamorphosed by post-Triassic 'tin granites')
Kudrass, H.R. & H.U. Schluter (1994)- Development of cassiterite-bearing sediments and their relation to Late
Pleistocene sea-level changes in the Straits of Malacca. Marine Geol. 120, p. 175-202.
(Survey of tin-bearing sediments in central parts of Straits of Malacca by seismic profiling and vibrocoring.
Placer deposits found in tidal scour channel of Cape Rachado and Pleistocene river valley. Cassiterite derived
from local primary mineralization of granite and from long-distance fluvial transport)
Kusnama, K. Sutisna, T.C. Amin & Sidarto (1995)- Geology of the Batam and Bintan area. Geol. Res. Dev.
Centre, Bandung, Bull. 18, p. 56-67.
(Batam and Bintan islands, S of Singapore. Outcrops of Permo-Carboniferous Berakit Fm metamorphics,
intruded by Late Triassic 'tin granites' (~225-230 Ma). Unconformably overlain by latest Triassic fluvialshallow
marine Duriangkang Fm sands-shales with 'Bintan flora' (see also Wade-Murphy et al. 2008),
?Jurassic redbeds, E Cretaceous Pancur Fm and Late Cretaceous Semarung Fm clastics)
Bibliography of Indonesia Geology v. 4.1 133 www.vangorselslist.com July 2012