摘要
应用 P 波初动半周期直接测定环境剪应力值的方法, 测定了北部湾61 ,62 级地震前后中小地震的环境剪应力值τ0 , 由此分析了北部湾地震过程的环境应力场特征。结果表明, 北部湾61 级地震后平均剪应力值较高, 达18 M Pa 左右; 62 级地震及两次5 级余震后剪应力值下降很快, 降至目前的6 M Pa 左右。
In this paper, the ambient shear stress values of the middle and the small earthquakes around the M 6 1 and 6 2 earthquakes in Beibuwan are determined by using the method of the P-wave first impulse half period. Therefore, the ambient stress field characteristics in Beibuwan earthquakes sequence are analyzed. The results show that the ambient shear stress average value is about 18 MPa after the M 6 1 earthquake in Beibuwan ,and the value decrease rapidly to 6 0 MPa after the M 6 2 and two M 5 0 earthquakes. Based on these, the tendency of seismic activity in the future in Beibuwan is estimated
出处
《华南地震》
1999年第2期25-31,共7页
South China Journal of Seismology
关键词
应力场
震源过程
环境剪应力
北部湾
地震序列
Stress field, Source process, Ambient shear stress, Beibuwan earthquake