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利用、振幅比资料测定澜沧—耿马震区中、小地震震源机制
引用本文:王绍晋,于利民,李钦祖.利用、振幅比资料测定澜沧—耿马震区中、小地震震源机制[J].地震研究,1991(3).
作者姓名:王绍晋  于利民  李钦祖
作者单位:云南省地震局,河北省地震局,河北省地震局 昆明,650041,石家庄,050021,石家庄,050021
摘    要:本文采用P、S最大振幅比资料测定中、小地震震源机制参数的方法,测定了澜沧—耿马地震前后震区182个中、小震的震源机制参数。并将这些结果结合大震及强余震震源机制P波初动解,对大震前后震区应力场方向的时空调整变化,以及序列的震源错动性质等进行了分析和讨论。

关 键 词:P、S振幅比  震源机制  澜沧—耿马地震

THE SOURCE MECHANISM OF MODERATE ANDSMALL EVENTS DETERMINED BY P AND S AMPLITUDERATIO IN LANCANG-GENGMA EARTHQUAKE AREA
Wang Shaojin.THE SOURCE MECHANISM OF MODERATE ANDSMALL EVENTS DETERMINED BY P AND S AMPLITUDERATIO IN LANCANG-GENGMA EARTHQUAKE AREA[J].Journal of Seismological Research,1991(3).
Authors:Wang Shaojin
Abstract:The source mechanism parameters of 182 moderate and small events in the seismic area before and after Lancang-Gengma Earthquake have been determined by the method of P and S maximum amplitude ratio. Combined the obtained results with the P first onsets of the event and its strong aftershocks the temporal-spatial variation of stress field direction in the seismic area before and after the event and the source dislocation properly of the sequence have been analysed and discussed.
Keywords:P and S amplitude ratio  Source mechanism  Luncang-Gengma earthquake
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