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The AAPG/Datapages Combined Publications Database

Journal of Petroleum Geology

Abstract

Journal of Petroleum Geology, Vol.13, No.1, pp. 93-112, 1990

©Copyright 2000 Scientific Press, Ltd.

THE CHAIDAM BASIN (NW CHINA): FORMATION AND HYDROCARBON POTENTIAL

Wang Qinmin* and M. P. Coward*

*Geology Department, Imperial College, London SW7 2BP.


Abstract

The Chaidam Basin, forms one of the deepest sedimentary basins in the world, with over 14 kms of sediment deposited since the Oligocene. Basement rocks consist of: (i) pre-Sinian gneisses; (ii) Sinian and Lower Palaeozoic sediments folded by the Silurian -- Devonian orogeny; (iii) Upper Paleozoic molasse in a Previous HithalfTop-graben produced by the collapse of the Silurian mountain belt; (iv) Carboniferous terrestrial to shallow-marine facies sediments deposited on the margins of Palaeotethys; and (v) Permo-Triassic sediments deposited in a back-arc basin N of the Palaeotethyan subduction zone.

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