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SEQUENCE STRATIGRAPHY AND SEA LEVEL CHANGES OF CAMBRIAN IN THE SOUTHERN MARGIN OF ORDOS BASIN

Cai Zhongxian (Department of Petroleum Geology, China University of Geosciences, Wuhan430074) Qin Yujuan (Hangzhou Institute of Petroleum Geology, Hangzhou310023) Jia Zhenyuan (Department of Petroleum Geology, Ch  
Researches and correlation of three outcrop sections in the southern margin of Ordos basin indicate that 14 third-order sequences can be recognized from Xinji Formation in Lower Cambrian to Fengshan Formation in Upper Cambrian, each of which generally includes 1~3 standard trilobita zones and has 2~3Ma duration except two Lower Cambrian sequences dated probably more than 5Ma. Subsidence analysis provides a representative exponential curve ( R 1 curve) which can be compared with Mckenzie's cooling plate model for passive margin, and good second-and third-scale of accommodation change curves ( R 2 curve and R 3 curve). R 2 curve is especially very similar to that of the Great Basin.
【Fund】: 国家基础性研究重大项目“中国古大陆及其边缘层序地层及海平面变化研究(SSLC)”资助
【CateGory Index】: P534.42
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