Active Features of the Hangingwall on the Listric Normal Fault Along the Southeastern Margin of Weihe Basin

作     者：Hou Jianjun,Bai Taixu,Liang Haihua,Zheng Wentao,and Wang ShiminDepartment of Geology,Peking University,Beijing 100871 China 

出 版 物：《Earthquake Research in China》 (中国地震研究（英文版）)

年 卷 期：1995年第9卷第3期

页      面：87-92页

学科分类：070904[理学-构造地质学] 0709[理学-地质学] 07[理学] 

基　　金：This Project is supported by the Fund for Excellent Young University Teachers of the State Education Commission of China 

主　　题：faulting listric fault finite element modeling Weihe Basin 

摘      要：Based on field observations and mechanic analysis,the authors think that synthetic faults,antithetic faults,and hangingwall cross-faults are formed on the piedmont alluvial-pluvial plain under the action of hangingwall blocks sliding downward and rotating along concave fault planes of the listric normal fault on the southeastern margin of Weihe *** characteristics of different movements and expressions on the surface of these structures may be taken as the main marks for listric normal fault segmentation.