摘要
使用了30个速报台站的观测数据,计算了100多个中国境内外的地震事件初至波走时残差。在此基础上分析各台所记录的所有地震事件的残差随方位角和震中距的分布,及产生这些残差的地球深部非流体静力平衡状态和地球表面构造等方面的原因,并给出了不同区域地震走时的平均校正值,从而提高了地震定位精度。
Using the observation data from 30 prompt stations,we calculated the arrival time resduals for 100 events occurred inside China and outside.Based on the above results,we analyzed the residual distribution with azimuthe and epicenter distance,discussed,from the viewpoints of the equilibrium of nonstatic forces and the earth surface structure,the reason why those residuals exist,and proposed the average correction for different regions,by which the precision of event locations can be improved.
出处
《地震地磁观测与研究》
1998年第4期48-54,共7页
Seismological and Geomagnetic Observation and Research
关键词
地震定位
走时残差
校正值
地震预报
地震台网
earthquake location
arrival time residual
correction
epicenter distance