通常断层崖的走向线平直,在断层崖被侵蚀的过程中随着横贯断层河谷的扩展,完整的断层崖被分割成不连续的断层三角面。而三角面的前面常形成一系列的冲积、洪积扇。
... escarp 内壕;筑陡坡 escarpment 陡坡,陡崖,峭壁;马头丘 fault escarpment 断层崖 ...
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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;
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.
我们初步利用扩散方程的这一特性来探讨断层崖坡面演化过程的可视化方法,同时预测其未来的形态。
The advantages of the diffusion equation feature are gained to discuss the visual process of scarp slope, together with forcasting it's future shape.
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。
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.
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