transform faults constitute the plate boundary parallel to the plate on both sides of the border for the strike-slip movement the stress is the shear conversion along the border neither the lithosphere hyperplasia or perish
转换断层构成沿边界两侧平行于板块的板块边界,走滑运动的应力是沿边界的剪切转换,既不是岩石圈增生也不是岩石圈消亡
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