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Some geologic signatures of fault creep in the continental area of China
引用本文:向宏发,虢顺民,张晚霞,张秉良.Some geologic signatures of fault creep in the continental area of China[J].地震学报(英文版),1997,10(1):115-122.
作者姓名:向宏发  虢顺民  张晚霞  张秉良
作者单位:HONG FA XIANG(向宏发) SHUN MIN GUO(虢顺民) WAN XIA ZHANG (张晚霞) BING LIANG ZHANG (张秉良)Institute of Geology,State Seismological Bureau,Beijing 100029,China
摘    要:SomegeologicsignaturesoffaultcrepinthecontinentalareaofChinaHONGFAXIANG(向宏发)SHUNMINGUO(虢顺民)WANXIAZHANG(张晚霞)BINGLIANGZHAN...

收稿时间:8 May 1995
修稿时间:8 September 1995

Some geologic signatures of fault creep in the continental area of China
Hong-Fa Xiang, Shun-Min Guo, Wan-Xia Zhang and Bing-Liang Zhang.Some geologic signatures of fault creep in the continental area of China[J].Acta Seismologica Sinica(English Edition),1997,10(1):115-122.
Authors:Hong-Fa Xiang  Shun-Min Guo  Wan-Xia Zhang and Bing-Liang Zhang
Institution:(1) Institute of Geology, State Seismological Bureau, 100029 Beijing, China
Abstract:Various geologic signatures of fault creep along most of the active faults in the continental area of China can be recognized, although no surface deformation caused by creep slip event has been observed. These signatures include ordered regional taphrogeny, linear deformation zones distributed along the fault, and seismic slip rate much lower than the geologic slip rate, etc. The recognition and identification of this important fault behavior are of great theoretical and practical significance.
Keywords:fault creep  continental area of China  geologic signatures
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