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用两个台上的S波位移求震源地方岩体錯动的方向
引用本文:郭增建.用两个台上的S波位移求震源地方岩体錯动的方向[J].地球物理学报,1960,9(1):20-24.
作者姓名:郭增建
作者单位:中国科学院地球物理研究所
摘    要:这种方法的基本根据是:(一)震源地方岩体錯动的方向与横波离源时的方向、横波离源时的射綫方向在一个平面內;(二)横波在传播过程中,β角变化很小. 推导了由S波β角求横波离源时位移方向的公式.由两个台上的S波β角就可分別求得两个横波离源时的位移面,这两个面的交綫就是震源地方岩体錯动的方向。討論了在烏尔夫网上具体运用这一方法的作图.这就大大地簡化了求解的过程,便于大量处理数据。

关 键 词:横波  位移方向  震源球  岩体  震源机制  方位角  地震台  入射面  投影  水平面  

FAULT-PLANE DETERMINATION BY MEANS OF 5-WAVES RECORDED AT TWO STATIONS
KUO TSENG-CHIEN.FAULT-PLANE DETERMINATION BY MEANS OF 5-WAVES RECORDED AT TWO STATIONS[J].Chinese Journal of Geophysics,1960,9(1):20-24.
Authors:KUO TSENG-CHIEN
Institution:Institute of Geophysics and Meteorology, Academia Sinica
Abstract:The method proposed here is based on the following facts: (1) At the focus, the direction of movement of the rock masses, the displacement of the S waves and the direction of the rays of the S waves all lie in one plane; and (2) the variation of the angle β in the course of propagation is very small. A formula is derived for finding the direction of displacement of the S wave on leaving the focus in terms of the angle β. From the β's obtained at two stations, it is possible to determine the planes of vibration of two S waves, whose intersection gives the direction of movement of the rock masses. The application of the method by use of Wulff s projection is also discussed.
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