The strike, dip, dip angle and position of a fault can directly been gotten by GPR records profiles, but the method cannot be used to describe the features of the fillings in fault plane.
通过雷达记录剖面可以直接探测得到断层走向、倾向、倾角及位置，但不能查明断层面内充填物的具体情况。
In this paper, a method is proposed such that the strike, dip, dipping direction and fracture length of a fault plane can be determined using of isoseismal lines.
本文提出了利用等震线测定地震断层面的走向、倾向、倾角和破裂长度等震源参数的宏观方法。
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