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Cai Xuelin;Wu Decha;Wei Xianguio  
Since the formation of East Qinling composite mountain chain due to B-subduction and collision between North China Plate and Yangzi Plate,tectonic movement of this region has never been still,and A-subduction and great slip-nappe has occured. On the basis of analysis of geology of the terrene and two-dimensional velocity of the earth's crust, the slip-nappe structure of East Qinling orogenic zone is studied,and a model of A-subduction of this region is suggested. It is considered that there are five or six separate-slips, several large scale nappe structures and two great A-subduction zones in this region. The A-subduction is characterized by "two wedge cleaving bamboo".
【Fund】: 国家自然科学基金
【CateGory Index】: P542.4
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