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长江三峡仙女山断层带的变形结构及其动力学分析
引用本文:吴树仁 刘子忠. 长江三峡仙女山断层带的变形结构及其动力学分析[J]. 地震地质, 1994, 16(3): 217-228
作者姓名:吴树仁 刘子忠
作者单位:中国地质大学,长江水利委员会三峡区勘测大队,中国地质大学
摘    要:根据仙女山断层分带性、分段性、分层性和断层变形结构特征,建立了其空间变形结构模式,进而讨论了仙女山断层带时间演化系列中两个主要变形阶段的几何学和运动学特征,并利用断层带的共轭节理、断面擦痕和显微构造标志分别确定燕山主期和喜马拉雅主期构造应力方向和差异应力大小,获得了若干重要的动力学资料

关 键 词:仙女山断层带  断层变形结构  差异应力  长江三峡

THE DEFORMATIONAL STRUCTURES AND DYNAMIC ANALYSIS OF XIANNUSHAN FAULTT ZONE IN THE CHANGJIANG RIVER GORGE AREA
Wu Shuren,Liu Zizhong,Qin Xingli,LiDonglin. THE DEFORMATIONAL STRUCTURES AND DYNAMIC ANALYSIS OF XIANNUSHAN FAULTT ZONE IN THE CHANGJIANG RIVER GORGE AREA[J]. Seismology and Geology, 1994, 16(3): 217-228
Authors:Wu Shuren  Liu Zizhong  Qin Xingli  LiDonglin
Abstract:On the basis of zonations segmentation and layering of the Xiannushan fault zone,a spatialdeformational structure model has been established,and geometrical and kinematic characteristicsof the fault in two main deformational stages of its temporal evolution sequence are discussed. Interms of conjugate joints, striations on fault planes and microstructure in fault zone,the tectonicstress directions and differential stress in main Yanshanian tectonic deformation and main Hi-malayan phases tectonic deformation have been determined, respectively,and some important dy-namic information has been obtained
Keywords:Xiannushan fault zone  Fault deformational structure  Differential stress  Changjiang Three Gorges China University of Geosciences(Wuhan).Wuhan430074.Water conservancy Committee for Yangtz river  Yichang 443000
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