Structure of the lithosphere and Mesozoic sedimentary basins in western Liaoning, northern Liaoning, and Songliao, northeast China
The western Liaoning, northern Liaoning, and Songliao areas represent three different tectonic units with different lithosphere thermal-mechanical properties in terms of composition, thickness of the thermal lithosphere, effective elastic thickness, depth of the detachment surface, and strength of the lithosphere. Western Liaoning is characterized by a thick lithosphere with high rigidity and strength, whereas Songliao and northern Liaoning are characterized by relatively thin lithosphere with low rigidity and strength. These differences controlled the development of distinct types of basins under an extensional regime during the Early Cretaceous. The basins in western Liaoning are controlled by faulting rather than by thermal subsidence. The Songliao basin in controlled both by faulting and by thermal subsidence, and thus both syn- and post-rift sequences developed with the same thickness in the center of the basin. In contrast, in northern Liaoning, the basins are mainly controlled by faulting, and to a lesser extent by subsequent thermal subsidence. As a part of east China, where more than 93% of the proven oil reserves of China are distributed, the western Liaoning-northern Liaoning-Songliao area also has attracted considerable attention for this hydrocarbon potential. The Songliao basin is proven to be the largest non-marine petroliferous basin and one of the most important oil- and gas-producing basins in China. In addition, the Tieling-Changtu basin and the Zhezhong depression in northern Liaoning show some petroleum potential. In contrast, basins in western Liaoning represent a limited prospect for oil and gas.
- Research Organization:
- Curtin Univ. of Technology, Perth (AU)
- OSTI ID:
- 20062587
- Journal Information:
- International Geology Review, Vol. 42, Issue 3; Other Information: PBD: Mar 2000; ISSN 0020-6814
- Country of Publication:
- United States
- Language:
- English
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