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《Geotectonica Et Metallogenia》 2011-02
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Formation and Tectonic Evolution of the Paleozoic Central Paleouplift of Ordos Basin and its Implications for Oil-Gas Exploration

DENG Kun1,2,ZHANG Shaonan1,ZHOU Lifa3 and LIU Yan4(1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,Sichuan,China;2.Shandong Provincial Key Laboratory of Depositional Mineralization and Sedimentary Minerals,Qingdao 266510,Shandong,China;3.Department of Geology,Northwest University,Xi′an 710069,Shaanxi,China;4.Changqing Oil Field Branch,CNPC,Xi′an 710021,Shaanxi,China)  
The tectonic evolution of the Paleozoic Central Paleouplift in Ordos Basin is reconstructed based on the comprehensive analyses of the stratigraphic thickness,tectonic evolution since Ordovician,and Paleozoic tectonic settings. Three major episodes of tectonic evolution can be recognized:(1) the initiation stage,as demonstrated by the formation of the relatively independent Central Uplift in the Middle Cambrian;(2) the growth stage,the long-term extrusion and rising as exhibited by the occurrence of the Low Ordovician Majiagou Formation;and,(3) the adjustment and decay stage,in which the substantial vatiations of structural and tectonic settings of the Paleouplift that is evidenced by the occurrence of the Carboniferous Benxi Formation and Permian Shanxi Formation. The Central Paleouplift controls the oil and gas accumulation in the region because it influences the sedimentation processes,formation of depression for hydrocarbon generation and accumulation,formation of caprock and traps,and thus the migration and storage of oil and gas.
【Fund】: 国家重点基础研究发展项目(973项目)(2003CB214601)资助
【CateGory Index】: P618.13
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