Zhang Bingling, Fang Zhongjing, Duan Ruitao, Xiang Hongfa. MICROSTRUCTURAL FEATURES OF GOUGES AND THEIR IMPLICATON IN CHENGGEZHUANG FAULT[J]. North China Earthquake Sciences, 1996, 14(4): 31-39.
Citation:
Zhang Bingling, Fang Zhongjing, Duan Ruitao, Xiang Hongfa. MICROSTRUCTURAL FEATURES OF GOUGES AND THEIR IMPLICATON IN CHENGGEZHUANG FAULT[J]. North China Earthquake Sciences, 1996, 14(4): 31-39.
Zhang Bingling, Fang Zhongjing, Duan Ruitao, Xiang Hongfa. MICROSTRUCTURAL FEATURES OF GOUGES AND THEIR IMPLICATON IN CHENGGEZHUANG FAULT[J]. North China Earthquake Sciences, 1996, 14(4): 31-39.
Citation:
Zhang Bingling, Fang Zhongjing, Duan Ruitao, Xiang Hongfa. MICROSTRUCTURAL FEATURES OF GOUGES AND THEIR IMPLICATON IN CHENGGEZHUANG FAULT[J]. North China Earthquake Sciences, 1996, 14(4): 31-39.
MICROSTRUCTURAL FEATURES OF GOUGES AND THEIR IMPLICATON IN CHENGGEZHUANG FAULT
Chenggezhuang fault is an east-branching fault of Mafang-Xiadian fault belt. A ccomprehensive study, such as microstructure of gouges, observation of SEM quartz fragment and TL dating of the fault gouges, gives the result that the last movement mode is stick slip mainly in different segment and the movement mode and intensity are different in each segment during different geological period.
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