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四川瀑布沟地区断裂破碎带的物质成分与断裂活动年代
引用本文:冯锦江,胡碧如,牛娈芳,张秉良.四川瀑布沟地区断裂破碎带的物质成分与断裂活动年代[J].地震地质,1988,10(1):87.
作者姓名:冯锦江  胡碧如  牛娈芳  张秉良
作者单位:国家地震局地质研究所 (冯锦江,胡碧如,牛娈芳),国家地震局地质研究所(张秉良)
摘    要:本文主要研究断层泥中新生的粘土矿物特征,并研究断层泥中石英碎砾表面溶蚀的显微形貌结构特征。粘土矿物以X-射线衍射分析为主,石英碎砾则利用扫描电子显微镜对其显微形貌结构进行分析,并根据石英表面溶蚀的形貌特征来探讨断裂活动的相对年代

关 键 词:四川  粘土  断层泥  石英碎屑  粒度

MATERIAL COMPOSITION OF THE FAULTED AND FRACTURED ZONE AND DETERMINATION OF THE AGE OF FAULTING IN THE PUBUGOU AREA, SICHUAN PROVINCE
Feng Jin-jiang,Hu Bi-ru,Niu Luan-fang and Zhang Bing-liang.MATERIAL COMPOSITION OF THE FAULTED AND FRACTURED ZONE AND DETERMINATION OF THE AGE OF FAULTING IN THE PUBUGOU AREA, SICHUAN PROVINCE[J].Seismology and Geology,1988,10(1):87.
Authors:Feng Jin-jiang  Hu Bi-ru  Niu Luan-fang and Zhang Bing-liang
Abstract:In this paper, characteristics of neogenic clay minerals and micro-surface texture of quartz fragment in fault gouge are discussed. Clay minerals are analysed mainly by X-ray diffraction, whereas miero-surface texture of quartz fragments is studied by SEM. The relative age of faulting is determined with the analysis of corroded surface texture of quartz fragments.
Keywords:Sichuan Province  Clay  Fault gouge  Quartz -fragment  Grain size  
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