| 注册
首页|期刊导航|地震地磁观测与研究|2010年河津MS 4.8地震前后单台波速比变化特征分析

2010年河津MS 4.8地震前后单台波速比变化特征分析

李丽 宋美琴 吴昊昱 李宏伟

地震地磁观测与研究2016,Vol.37Issue(1):8-14,7.
地震地磁观测与研究2016,Vol.37Issue(1):8-14,7.DOI:10.3969/j.issn.1003-3246.2016.01.002

2010年河津MS 4.8地震前后单台波速比变化特征分析

Temporal variation of vP/vS at single seismic station before and after Hejin MS 4.8 earthquake in the year 2010

李丽 1宋美琴 2吴昊昱 1李宏伟2

作者信息

  • 1. 中国太原030021山西省地震局
  • 2. 中国山西030025太原大陆裂谷动力学国家野外科学观测研究站
  • 折叠

摘要

Abstract

Based on the seismic phase report of Shanxi Province from January 2001 to October 2014, the variation of wave velocity ratio before and after Hejin MS 4.8 earthquake in the year 2010 is analyzed by using Wadati method of single station and multi-earthquake in this paper. And four stations,those with relatively continuous seismic phase data,were selected. The results showed that the middle wave velocity ratio displayed anomaly for two or three years at Linfen Seismic Station and Anze Seismic Station,which are situated in the northern side of Hejin MS 4.8 earthquake’s epicenter. At the same time,the different azimuthal partition result indicated that, the wave velocity ratio curve,which represented southwest of Linfen Seismic Station and south of Xixian Seismic Station,showed short period anomaly before Hejin MS 4.8 earthquake. The abnormity had obvious relationship with scope of earthquake pregnancy,the better ray the station accepted,the more obvious anomaly was showed.

关键词

河津MS 4.8地震/波速比/孕震区/单台多震和达法

Key words

Hejin MS 4.8 earthquake/wave velocity ratio/seismogenic zone/Wadati method of single station and multi-earthquake

引用本文复制引用

李丽,宋美琴,吴昊昱,李宏伟..2010年河津MS 4.8地震前后单台波速比变化特征分析[J].地震地磁观测与研究,2016,37(1):8-14,7.

基金项目

地震科技星火计划青年项目(XH14010Y)、山西省地震局青年科研项目(SBK-1412)和2016年度震情跟踪定向工作任务(2016010106)联合资助 ()

地震地磁观测与研究

1003-3246

访问量3
|
下载量0
段落导航相关论文