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.
鉴于倾斜方向的变化，此地可能存在一个局部的背斜褶皱。
In view of the variation in the dip, here could be a local anticlinal fold.
由于受区域构造长期作用的影响，在北天山山前地区逐步发育形成了多排褶皱背斜及活动断裂，且运动方式具有独特性。
Under the effect of regional tectonics there develop many raws drape anticline and active fault in the front of mountain and they have especial motion fashion.
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