The analysis of seismic data comes to the conclusion that the shortening of formations in a compressional basin mainly results from faulting and folding.
由地震资料分析认为，造成压性盆地地层缩短的原因主要有两方面：①断裂作用；②褶皱作用。
The analysis of seismic data comes to the conclusion that the shortening of formations in a compressional basin mainly results from faulting and folding.
由地震资料分析认为，造成压性盆地地层缩短的原因主要有两方面：①断裂作用；②褶皱作用。
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