picture geometry fault 图象几何畸变
Each segment has a distinctive difference of its own in fault geometry, associated structures, active age and the sedimentation control etc.
各分段断层的结构、形态、伴生构造、活动时间及对沉积作用的控制等都存在较明显差异。
But to the region of nappe structure, by the reason of rising reverse fault top wall, so we just can calculate the fault geometry under the footwall breakpoint.
而对于逆断层因其上盘的上升过程，使得推算的断层只能获取下盘断点以下的构造形态。
Examining the geometry of fault zones offers clues to the level and the direction of the stress exerted on the rock.
考察断层系统的几何分布可以推断出岩石所受的应力大小和方向。
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