And some relevant geologic data regression equations for fault scarp formed in the past 2700 years have been obtained.
获得了相应地区断层陡坎的一些资料和距今2700年左右形成的断层陡坎回归方程。
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。
The frontal riser of the first pediment surface (P1) is the most recent fault scarp or diluvial platform; at the foot of pediment P1 outcrops the fault.
第1级麓原面(P1)的前缘陡坎为最新断层崖或洪积台地,断层崖的坡脚为断裂带地表出露位置;
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