摘要
在地震子波理论的基础上，研究了典型断层情况下地震子波波形变化的规律，从理论上证明了当地震波通过断层时，子波波形变化比走时对断层的反应更为敏感。实测资料的分析计算结果表明。
In this paper,on the basis of theory of seismic wavelet, regulations of wavelet form variation have been studied in typical fault. It is proved from theory that when seismic waves pass through faults, wavelet form variations are more sensitive than travel time on faults. The results from observation data demonstrate that it is practicable to judge fault properties by seismic wavelet theory.
出处
《西北地震学报》
CSCD
1996年第3期54-59,共6页
Northwestern Seismological Journal
关键词
地震波形
断层性状
波形变化
地震子波
地震波
Fault behavior, Seismic wave form, Wave form variation, Seismic wavelet
