The method of reflectivity in the calculation of synthetic seismograms is extended for the case of a point shear dislocation source buried in a layered medium.
本文将计算综合地震图所用的反射法，推广于层状介质中的剪切位错内源情况。
The method of reflectivity in the calculation of synthetic seismograms is extended for the case of a point shear dislocation source buried in a layered medium.
本文将计算综合地震图所用的反射法，推广于层状介质中的剪切位错内源情况。
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