节点文献

北部湾地震的震源机制及地震地质条件

FOCAL MECHANISM AND SEISMIC GEOLOGIC CONDITIONS OF THE BEIBUWAN EARTHQUAKES

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 尹克坚吴时平王林

【Author】 Yin Kejian;Wu Shiping;Wang Lin(Seismological Bureau of Guangxi Zhuang Autonomous Region,Nanning 530022)

【机构】 广西壮族自治区地震局

【摘要】 对北部湾地震的震源机制解和地震地质条件进行了详细分析,认为靖西-崇左断裂带过震中的北北西向断层为发震断裂;四会-吴川断裂带过震中的北东东向断层为控震构造。震源构造应力场的主压应力方向为北西-南东向,发震断层的活动方式既有垂直差异运动又有走滑运动。

【Abstract】 The focal mechanism solution and seismic geologic conditions of the Beibuwan earthquakes are discussed.The fault which belongs to Jingxi-Chongzuo fault zone in NW-SE direction and crosses the epicenter is the seismogenic fault.The fault which belongs to Sihui-Wuchuan fault zone in NE-SW direction and crosses the epicenter must have some effects on this seismic sequence.The main pressure direction of the focal stress field is in NW-SE direction.The Beibuwan basin and the fault in and around it inherit the past active model still now.

  • 【文献出处】 华南地震 ,SOUTH CHINA JOURNAL OF SEISMOLOGY , 编辑部邮箱 ,1996年03期
  • 【分类号】P315.3
  • 【被引频次】14
  • 【下载频次】171
节点文献中: 

本文链接的文献网络图示:

本文的引文网络