摘要
本文从地质构造、波列特征、P波初动、S-P到时差、主要震相、最大振幅、震中距等方面着手对沈阳台记录到的中、强震进行分析,力求归纳出国内和国外不同区域的波形和震相特征。
The paper analyzes the geological structure,features of seismic wave train,P-wave first motion,arrival S-P time difference,major seismic phase,maximum amplitude,epicentral distance,etc.Analyzed on the moderate earthquakes recorded by Shenyang seismic station,the characteristics of seismic waveform and phases in different districts domestic and foreign can be summarized.
引文
[1]贾庆华,陈贵美,国内5.O级以上地震数字记录波形及震相特征分析,华南地震[J].2004(3):57-64.
[2]邵中明,胡洪,李峰,甚宽频带数字记录分析方法武,台站通讯,(91):16-30.
[3]陈建军,许玉红等,震相分析在高台地震台数字地震观测中的应用,地震地磁观测研究[J].2004(3):75-80.