通过勘探地震信息可以看出：中国西部推覆前锋带的拆离型、褶皱型、前冲型、反冲型等前锋构造。
Through the exploration, earthquake information, we can reach the nappe leading structure modes in the West of China including fold, advance, recoil and so on.
可划分为伸展变形、冲断褶皱变形、拆离滑脱变形等3种构造变形样式。
The deformation style includes 3 types: stretching deformation, thrust fold deformation and decoupling slip deformation.
核杂岩表现为多重拆离，南翼主拆离断层系控制了山前坡地地貌，北翼拆离系发生褶皱并呈分叉状。
The master detachment fault system at the southern side controls the geomorphology of the piedmont slopes, whereas the detachment system at the northern side is folded and sprays out.
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