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赣北地区中小地震震源机制分析

陈浩 肖孟仁 项月文 李传江

地震地磁观测与研究2017,Vol.38Issue(6):21-25,5.
地震地磁观测与研究2017,Vol.38Issue(6):21-25,5.DOI:10.3969/j.issn.1003-3246.2017.06.004

赣北地区中小地震震源机制分析

Analysis on the focal mechanism of medium-small earthquakes in the northern area of Jiangxi Province

陈浩 1肖孟仁 1项月文 1李传江1

作者信息

  • 1. 中国 南昌 330036 江西省地震局
  • 折叠

摘要

Abstract

Using the method of Snoke, focal mechanism solution for 11 medium-small earthquakes with ML≥3.0 were calculated in northern area of Jiangxi Province since 2008 to 2015. The result showed thatP axis andT axis accorded with tectonic stress ifeld in this area. In the northern area of Jiangxi Province, tectonic stress ifeld was composed by compressive stress in EW direction and tensile stress in NS direction. Fault zones were dominated by strike-slip fault and normal fault. Jiujiang-Ruichang area was controlled by Xiangfan-Guangji fault zone and Tanlu fault zone, it was easy to take the strike-slip earthquakes under tectonic stress ifeld with stability direction.

关键词

Snoke方法/震源机制/构造应力场/断裂带

Key words

focal mechanism/ifrst motion/amplitude ratio/tectonic stress ifeld/fault zone

引用本文复制引用

陈浩,肖孟仁,项月文,李传江..赣北地区中小地震震源机制分析[J].地震地磁观测与研究,2017,38(6):21-25,5.

基金项目

测震台网青年骨干培养专项(项目编号:20160515) (项目编号:20160515)

地震地磁观测与研究

1003-3246

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