用宽频带波形资料研究青海西捷6.8级地震的震源过程  

A STUDY ON SOURCE PROCESS OF M S 6.8 EARTHQUAKE IN XIJIE, QINGHAI PROVINCE OF NOVEMBER 5,1988 BY USING BROADBAND DIGITAL SEISMIC WAVE DATA

作　　者：刘振[1] 周蕙兰[1] 

机构地区：[1]中国科技大学研究生院

出　　处：《地震地质》1998年第3期219-224,共6页Seismology and Geology

基　　金：中国科学技术大学科研基金;国家学科博士点基金

摘　　要：利用中国数字地震台网（ＣＤＳＮ）的宽频带数字化波形资料进一步研究了１９８８年１１月５日青海省西捷ＭＳ６．８级强震的震源过程。通过波形模拟和基于优化遗传算法的全局反演，对该地震的震源参数和破裂特征进行了分析。初步结果表明，此强震是以一次主破裂为特征的事件，与略带逆掩分量的走滑活动断层有关。根据单向破裂对各台站视震源时间函数的影响的分析，认为破裂可能是沿北西走向的断层面由东南向西北传播。The broadband seismic wave data of CDSN are used to make a further study on the source process of the Qinghai, Xijie M S 6.8 earthquake on November 5, 1988. With the waveform fitting and global searching algrithm based on the optimized Genetic Algorithm, the source parameters and rupture characteristics are analyzed. The results show that this earthquake is an event dominated by one rupture and associated with a strike slip active fault which has slightly overthrust component. In the light of analyses for the effect of rupture direction upon the station quasi source time function, it is suggested that the rupture was likely to spread from SE to NW along the NW trending fault plane.

关 键 词：震源过程 波形反演 遗传算法 宽频带波形 地震 

分 类 号：P315.3[天文地球—地震学]