伊犁地块的南、北缘边界在二叠纪期间经受了走滑作用的强烈改造。
The two boundaries of the Yili Block have been reworked by the Permian strike-slip faulting.
这个走滑拉分盆地的中部发育伸展构造，这些伸展构造是由走滑作用派生而来的。
The extensional structures developed in the central Bohai Bay basin are induced by strike slip.
在一些走滑断层产生于聚敛地壳内或处于转换挤压作用下的地区内，岩石向上断裂成一种正向花状构造。
In areas where strike-slip faults occur in converging crust, or transpression, rocks are faulted upward in a positive flower structure.
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