高陡背斜带属隔挡式平行褶皱，纵向变异很大，形成多种圈闭类型，具有不同的气、水分布规律。
The high-steep anticline belt belonged to barrier parallel fold is greatly variant in vertical, forming many types of traps and being of various gas-water distribution laws.
这种有序变形规模巨大，仅川东的隔挡式褶皱冲断带规模就超过了著名的侏罗山式褶皱。
This regulated deformation is considerable in scale, and hence the partition wall style fold-thrust belt in the east of Sichuan is much bigger than the famous Jurassic style folding.
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