Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
Sumatra, Sunda Shelf, Natuna - Bibliography of Indonesia Geology
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Bothe, A.C.D. (1925)- Het voorkomen van tinerts in den Riau archipel en op de eilanden van Poelau Toedjoeh<br />
(Anambas en <strong>Natuna</strong> eilanden). Verslag. Meded. Indische Delfst<strong>of</strong>fen en Hare Toepassingen, Dienst Mijnbouw<br />
Nederl.- Indie 18, p. 1-42.<br />
(‘The occurrence <strong>of</strong> tin ore in the Riau Archipelago and the Anambas and <strong>Natuna</strong> islands’. Widespread<br />
indications <strong>of</strong> cassiterite ore, but no large deposits. Includes presence <strong>of</strong> Upper Triassic Halobia-bearing<br />
shales. With maps <strong>of</strong> islands <strong>of</strong> Karimon, Kundur, Bintan, Lingga, Batam and Anambas- <strong>Natuna</strong>. <strong>Geology</strong><br />
described in more detail in Bothe 1928)<br />
Bothe, A.C.D. (1928)- Geologische verkenningen in den Riouw-Lingga archipel en de eilandengroep der<br />
Poelau Toedjoeh (Anambas en Natoena eilanden). Jaarboek Mijnwezen Nederl.-Indie 54 (1925), Verhand. 2, p.<br />
101-152.<br />
(‘Geological reconnaissance in the Riau-Lingga Archipelago and Anambas and <strong>Natuna</strong> islands’.)<br />
Cissarz, A. & F. Baum (1960)- Vorkommen und Mineralinhalt der Zinnerzlagerstatten von Bangka<br />
(Indonesien). Geol. Jahrbuch 77, p. 541-580.<br />
('Occurrence and mineral content <strong>of</strong> tin ore deposits <strong>of</strong> Bangka, <strong>Indonesia</strong>'. Primary tin mineralization<br />
associated with Young Cimmerian granites in Triassic sediments)<br />
Collette, B.J. (1954)- On the gravity field <strong>of</strong> the <strong>Sunda</strong> region. Geol. Mijnbouw 16, p. 271-300.<br />
De Groot, C. (1887)- Herinneringen aan Blitong, historisch, lithologisch, mineralogisch, geographisch,<br />
geologisch en mijnbouwkundig. H.L. Smits, The Hagua, p. 1-549.<br />
('Memories <strong>of</strong> Belitung, historic, lithologic, mineralogic, geologic and mining'. One <strong>of</strong> oldest reports on<br />
geology and tin mining on Billiton/ Belitung island by mining engineer De Groot)<br />
De Neve, G.A. & W.P. de Roever (1947)- Upper Triassic fossiliferous limestones in the island <strong>of</strong> Bangka. Proc.<br />
Kon. Nederl. Akad. Wetensch., Amsterdam, 50, 10, p. 1312-1314.<br />
(online at: http://www.dwc.knaw.nl/DL/publications/PU00018447.pdf)<br />
(Upper Triassic low metamorphic limestones below Loemoet mine tin deposits, SE <strong>of</strong> Klabat Bay, folded with<br />
phyllites and fine-crystalline quartzites. First documentation <strong>of</strong> poorly preservled Norian corals (Montlivaltia<br />
molukkana), calcareous sponges (Peronidella moluccana) and crinoids (Entrochus spec., Encrinus). No<br />
illustrations)<br />
De Roever, W.P. (1950)- Over een door oplossing van kalksteen gevormde depressive in het kongoppervlak op<br />
Banka, waarin een grote hoeveelheid tinerts is geaccumuleerd (mijn 7 der Sectie Belinju). De Ingen. in<br />
<strong>Indonesia</strong>, IV, 2, 3, p. 6-16.<br />
('On a depression in the kong surface <strong>of</strong> Bangka formed by dissolution <strong>of</strong> limestone, in which a large quantity <strong>of</strong><br />
tin ore accumulated (mine 7 <strong>of</strong> Belinju sector)')<br />
De Roever, W.P. (1951)- Some additional data on the stratigraphy <strong>of</strong> Bangka. Geol. Mijnbouw 13, 10, p. 339-<br />
342.<br />
(New fossil finds on Bangka Island include: Upper Triassic in limestone bed in dynamo-metamorphic clastics<br />
and volcanics in Lumut tin mine (coral Montlivaltia molukkana Wanner, sponges Peronidella moluccana<br />
Wilckens and crinoids). Also Permian white silicified limestone interbedded in phyllite-sandstone series with<br />
fusulinids in old tin mine 17 at at Airduren, NE Bangka, including )<br />
Dickerson, R.E. (1941)- Molengraaff river; a drowned Pleistocene stream and other Asian evidences bearing<br />
upon the lowering <strong>of</strong> sea level during the ice age. Proc. Univ. Penn. Bicent. Conf., p. 13-24.<br />
(In Pleistocene a great river, here named Molengraaff River, flowed N between Malay Peninsula and Borneo,<br />
with its headwaters in <strong>Sumatra</strong>. Evidenced by distribution <strong>of</strong> similar fresh- water fish species in E <strong>Sumatra</strong> and<br />
W Kalimantan and configuration and sediments <strong>of</strong> drowned valley. Sea level was lowered by 240-300’ during<br />
last glaciation)<br />
<strong>Bibliography</strong> <strong>of</strong> <strong>Indonesia</strong> <strong>Geology</strong> v. 4.1 128 www.vangorselslist.com July 2012