The left-lateral strike-slip movement of the Zhongwei fault zone since late Pleistocene caused the differentiation of preexisting overthrust faults in the zone.
青藏高原东北缘的中卫断裂带在晚更新世以来的左旋走滑运动中，先存的挤压逆掩、逆冲断裂带发生了分化。
2
The secular GPS crustal deformation image has reflected the relatively complete leftlateral strike slip movement of this active fault zone.
长趋势GPS地壳形变图像反映了这条活动断裂带相对完整的左旋走滑活动。
3
The focal mechanism is mainly left-lateral strike-slip, with a small thrust component.