Patterns of Clay Minerals Transformation in Clay Gouge, with Examples from Revers Fault Rocks in Devonina Niqiuhe Formation in The Dayangshu Basin  

作　　者：MENG Jie LI Benxian ZHANG Juncheng LIU Xiaoyang 

机构地区：[1]College of Earth Science,Jilin University,Changchun,Jilin 130012 [2]State Key Laboratory of Inorganic Synthesis and Preparative Chemistry,Jilin University,Changchun,Jilin 130012 [3]College of Geographic Science,Harbin Normal University,Harbin,Heilongjiang 150025

出　　处：《Acta Geologica Sinica(English Edition)》2017年第S1期59-60,共2页地质学报（英文版）

基　　金：financed by the National Youth Sciences Foundation of China (No. 41502044)

摘　　要：The role of authigenic clay growth in clay gouge is increasingly recognized as a key to understanding the mechanics of berittle faulting and fault zone processes,including creep and seismogenesis,and providing new insights into the ongoing debate about the frictional strength of brittle fault(Haines and van der Pluijm,2012).However,neither the conditions nor the processes which

关 键 词：with Examples from Revers Fault Rocks in Devonina Niqiuhe Formation in The Dayangshu Basin Patterns of Clay Minerals Transformation in Clay Gouge 

分 类 号：P574[天文地球—矿物学]