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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2006-01
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Sedimentological responses of the coupling between tectonics and sequence since Indo-Chinese epoch in the southern margin of the eastern Qinling and Dabie orogenic belt,China

YAN Jin-quan~(1,2),GUO Zhan-feng~21.China University of Geosciences,Wuhan,Hubei 430074;2.Exploration & Development Research Institute of Jianghan Oilfield Branch Company,SINOPEC,Qianjiang,Hubei 433124  
Through comparing the tectonic sequences stratum of Triassic-Paleogene period in the east of Hubei,in Jingmen-Dangyang basin,in Zigui basin and in the northeast of Sichuan,on the southern margin of the eastern Qinling and Dabie orogenic belt,three main tectonic sequences are divided.This paper analyzes the coupled relationship between the characterized transition and transfer processes of depositional basins and orogenic belts of its surrounding area since Indo-Chinese epoch in the mid-upper Yangtze area.Through studying the stratigraphic framework of tectonic sequence,the characteristics of deposits and multi-episode tectonic movements show the eastern Qinling and Dabie orogenic movement and basin formation processes.
【Fund】: 中国石化股份有限公司科学技术开发研究项目(P02006)
【CateGory Index】: P542.3
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