乌尊硝段左旋走滑的断错地貌极为发育。
Along the Wuzunxiao segment, the left lateral dislocation landform is well developed.
晚更新世晚期以来的平均左旋走滑运动速率达10。
The average of its sinistral strike-slip movement since the late part of the late Pleistocene is up to 10.
震源机制主要是左旋走滑，带有很小的逆冲倾滑分量。
The focal mechanism is mainly left-lateral strike-slip, with a small thrust component.
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