摘要
利用矩张量反演方法反演了 1996年 6月 1日天祝 -古浪 5 .4级地震序列的震源机制 ,并与该区小震综合断层面解进行了比较。在此基础上讨论了该地震前后震源区应力场的变化特征。
The source mechnisms of the seismic sequence of Tianzhu Gulang earthquake(M5.4,June 1,1996)has been inverted using the method of seismic moment tensor,the results are compared with the ones of the synthetic fault plane solutions from the micro events in the area.On the basis of it the variation characteristics of stress field in the source area before and after the earthquake have been discussed.
出处
《高原地震》
2000年第2期37-42,共6页
Plateau Earthquake Research
基金
地震科学联合基金重点项目!( 95- 0 7- 436 )资助
关键词
矩张量反演
区域应力场
短临变化
震源区
地震
Moment tensor inversion
Synthetic fault plane solutions of micro earthquakes
Local stress field
Short term variation
