首页 | 本学科首页   官方微博 | 高级检索  
     

南秦岭房县拉分盆地的构造发育特征
引用本文:甘家思,刘锁旺,李愿军. 南秦岭房县拉分盆地的构造发育特征[J]. 大地测量与地球动力学, 2003, 23(4): 87-91
作者姓名:甘家思  刘锁旺  李愿军
作者单位:1. 中国地震局地震研究所,武汉,430071
2. 武汉大学土木建筑工程学院,武汉,430072
基金项目:地震科学联合基金 ( 880 15 )《南秦岭造山带走滑断裂、拉分盆地与地震活动研究》课题资助
摘    要:南秦岭新生代房县盆地是北西向安康-竹山-房县左旋走滑断裂构造带东南端拉分盆地。论述了该盆地边界断裂、盆地结构和3期盆地发育演化特征。估算盆地的最大扩张量为2.73km,主控边界断裂的走滑位错量为3.57km,并分析了盆地主要储能结构与地震的关系。

关 键 词:构造形变 地震 南秦岭 房县拉分盆地 盆地扩张量
文章编号:1671-5942(2003)04-0087-05
修稿时间:2002-12-22

TECTONIC DEVELOPMENT FEATURES OF FANGXIAN PULL-APART BASIN OF SOUTH QINLING
Gan Jiasi ),Liu Suowang ) and Li Yuanjun ) )Institute of Seismolog,CSB,Wuhan )School of Civil and Architectural Engineering of Wuhan University,Wuhan. TECTONIC DEVELOPMENT FEATURES OF FANGXIAN PULL-APART BASIN OF SOUTH QINLING[J]. Journal of Geodesy and Geodynamics, 2003, 23(4): 87-91
Authors:Gan Jiasi )  Liu Suowang )  Li Yuanjun ) )Institute of Seismolog  CSB  Wuhan )School of Civil  Architectural Engineering of Wuhan University  Wuhan
Affiliation:Gan Jiasi 1),Liu Suowang 1) and Li Yuanjun 2) 1)Institute of Seismolog,CSB,Wuhan 430071 2)School of Civil and Architectural Engineering of Wuhan University,Wuhan 430072
Abstract:The Fangxian basin of Cenozoic Era of South Qinling is a pull-apart basin at the southeastern end of the Ankang-Zhushan-Fangxian NW-trending left-lateral strike-slip fault zone.The boundary faults,basin structure and development and evolution features in three periods of this basin are described.The maximum expansion of this basin is estimated as 2.73 km,the strike-sliping dislocation of its principal boundary fault is 3.57 km and the relation of main energy-reserving structure of the basin with the earthquakes is analyzed as well.
Keywords:Fangxian pull-apart basin  tectonic deformation  earthquake  South Qinling  
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号