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《Acta Sedimentologica Sinica》 2004-04
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Discovery of Breakup Uncomnformity at the Top of Lower Sinian in the South Margin of North China Block: the Geological Implication

CAO Gao she 1,2,3 ZHANG Shan wen 2 LIU Zhong quan YANG Xiao yong 3 LIU De liang 3 ZHOU Song xing 4 YANG Qiang 3 1(Geologiocal Research Institute of Shengli Oilfield Company, Dongying,Shandong 257015)2(Research Center of Earth Science, Zhengzhou University,Zhengzhou 450052)3(University of Science and Technology of China, Hefei 230026) 4(Anhui Exploration Department of Jiangsu Bureau of Petroleum Exploration, Yangzhou, Jiangsu 225000)  
A film of pyrites was discovered on the interface of Lower Sinian Sidingshan Formation and Fengtai conglomerate, at Sishilichangshan Mountains in the south margin of the North China Block. The macroscopic, microscopic and geochemical studies of the film of pyrite reveal that the interface is a breakup unconformity. The discovery and determination of the breakup unconformity provides substantive proof for studying geological response of North China Block at the interval of Rodinia supercontinent breakup, and offers important tectonic background for studying the genesis of Fengtai conglomerate and its equivalence.
【Fund】: 中国科学院知识创新工程(KZCX2-107);; 胜利石油管理局联合资助
【CateGory Index】: P542.34
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