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湘东南地区地震构造环境分析
引用本文:肖和平,缪卫东.湘东南地区地震构造环境分析[J].大地测量与地球动力学,2010,30(Z1).
作者姓名:肖和平  缪卫东
作者单位:1. 湖南省地震局,长沙,410004
2. 武汉地震工程研究院,武汉,430071
基金项目:科技部科技支撑项目2006BA13B01
摘    要:从湖南省东南地区的大地构造、新构造特征及主要第四纪断裂活动研究入手,分析了区域地震构造环境,认为新构造运动期间,地壳运动以大面积整体性缓慢抬升为主要形式,兼有间歇性不均匀抬升活动;区域断裂多为第四纪活动断裂,并存在中更新世活动断裂,然而断裂的现今活动不甚明显,对区域地质构造的分割性和控制性较弱。

关 键 词:湘东南地区  地震构造环境  地壳运动  断裂  控制  

ANALYSIS OF SEISMOTECTONIC ENVIRONMENT IN SOUTHEAST OF HUNAN PROVINCE
Xiao Heping,Miao Weidong.ANALYSIS OF SEISMOTECTONIC ENVIRONMENT IN SOUTHEAST OF HUNAN PROVINCE[J].Journal of Geodesy and Geodynamics,2010,30(Z1).
Authors:Xiao Heping  Miao Weidong
Institution:Xiao Heping1) , Miao Weidong2)(1)Earthquake Administation of Hunan Province,Changsha 4100042)Wuhan Institute of Earthquake Engneering,Wuhan 430071)
Abstract:Starting with the research on the basic characteristics of tectonic,neotectonic and the activity of dominating Quaternary fault in the southeast of Hunan province,the regional seismotectonic environment was analyzed.It is recognized that during the neotectonic movement period,the crust has mainly undergonely entire and slowly elevated movement along with intermittence uneven elevated movement.The regional faults generally occured in the Quaternary and some in the mid-Pleistocene,but there are no distinctive...
Keywords:the southeast of Hunan region  seismotectonic evironment  crustal movement  fault  control  
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