这种类型的断层通常出现在挤压区域，比如像日本那样的，板块向另一板块之下俯冲的区域。
This type of faulting is common in areas of compression, such as regions where one plate is being subducted under another as in Japan.
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.
背斜褶皱的核部在断层间受到挤压，遭受到很强的破坏。
The core of the anticlinal fold, which is squeezed between faults, underwent intense crushing.
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