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Characteristics of Fault-Block Movement and Seismicity in the Weihe Basin
详细信息   
摘要
According to field investigation and previous information, this paper expounds the movements of active faults and present fault blocks in the Weihe Basin and challenges the attitude (dip angle) of the Qinling piedmont faults, raising a conception of the movement differentiation between the piedmont fault system of Beishan Mountains and the Qinling piedmont fault system.

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