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1.The fault scarp in ground surface approximately is along the fault face that consists of Cretaceous sandstone and Archaean gneiss.
断层陡坎与白垩系砂岩和太古界片麻岩之间的断层位置大致吻合。收藏指正
2.It is feasible to infer the specific shape of a fault scarp with the help of its average diffusion age and origin time of the scarp.
无论是单一型断层崖还是复合型断层崖，通过断层崖的平均扩散年龄和初始错断时间，就能推断出它在某一时刻的具体形态。收藏指正
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