Structural Traces of Secondary Faults(Fractures) along the Main Faults and Their Reliability as Kinematic Indicators

查看全文 作　　者：Jin [1]ZHANG;Jinyi [1]LI;Zongjin [2]MA;Wenjun [3]REN

机构地区：[1]Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;[2]Institute of Geology, China Earthquake Administration, Beijing 100029, China;[3]Department of Chang Qing Geophysical Survey, Geophysical Company Limited, China National Petroleum Corporation, Xi'an 710000, China

出　　处：《Acta Geologica Sinica(English Edition)》索引2011年第85卷第5期,共13页

基　　金：funded by the National Basic Research Progam of China(Nos. 2007CB411306 and 2001CB409810);China Geological Survey(No.1212010611806);the National Natural Science Foundation of China(No.40702032) 摘　　要：Secondary/minor structures occurring along the main fault surfaces are important indicators for judging the kinematic characteristics of faults.However,many factors can lead to the formation of these structures,which results in the difficulty for rapid judgment and application in the fields.A series of secondary faults/fractures developed due to the movement of main faults are the most important and widespread phenomena in the scope of brittle deformation.The morphology of the main fault surfaces is vari... 关键词：secondary fracture/fault kinematic indicator fault surface fluctuation

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Structural Traces of Secondary Faults(Fractures) along the Main Faults and Their Reliability as Kinematic Indicators

参考文献(32)

引证文献(5)

耦合文献(58)

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