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《Journal of Jiling University (Earth Science Edition)》 2004-03
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Evolution of paleogeography of Triassic of Lower Yangtze area

CHENG Ri-hui,BAI Yun-feng,LI Yan-bo (College of Earth Sciences,Jilin University,Changchun130061,China)  
Marine carbonate, marine-continental interbeded and continental sediments were accumulated in Lower Yangtze area during Triassic. The spatial distribution of sedimentary facies belts and the temporal changes of paleography were controlled by tectonics. Basin development and evolution in this area is related to the interactions of South China plate and Yangtze plate,as well as North China plate and Yangtze plate. Indochina movement occurred at the end of early-middle Triassic is the key control to the changes of tectonic-paleogeography, which led to the change from marine sedimentation to continental sedimentation. The characteristics of Triassic paleogeographic evolution of Lower Yangtze area also provide some sedimentary evidences for collision between Yangtze plate and North China plate.
【Fund】: 中国石化股份有限公司项目资助(P0000202-05);; 原长春科技大学创新人才基金项目资助(2000003)
【CateGory Index】: P531
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