犁式正断层也有称剥离断层(Denudational fault),它是一种倾角随深度变缓的低角度正断层,形态似犁状,故名为犁式正断层。其特点,上盘地层沿倾向下滑,较浅层位的年青岩层直接盖于较深层位的岩层之上,断层上陡,向下变平而联合成一个基底滑脱面,断层面 The plow-type normal fault is also known as the Denudational Fault. It is a low-angle normal fault whose dip angle decreases with depth and is shaped like a plow. It is called a plow-type normal fault. Its characteristics, the plate down the dip along the slope, the younger layer of shallow rock layer directly on top of the deeper layers of rock formation, the fault steep, flattened down and combined into a basement slip surface, the fault surface