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。
And some relevant geologic data regression equations for fault scarp formed in the past 2700 years have been obtained.
河流侵蚀形成陡坎的方向追随河流的冲沟方向，具不稳定性，并且陡坎的倾向沿河对称。
Direction of scarps caused by river erosion follows the river, is unstable and the tendency of scarps is symmetric along the river.
构造地貌能反映断裂的结构变形特征和断层的活动强度。例如断层陡坎的高度、长度和坡度以及断层陡坎的连续程度。
Tectonic topography can reflect the structural deformation feature and active strength of faults, such as the height, length and gradient of a fault scarp as well as its continuity.
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