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.
其构造变形经历了由隔槽式褶皱到“两背一断”，最终形成隔挡式褶皱的演化过程。
The structural deformation has experienced the evolution from trough like folds to "two anticlines with one fault", and finally formed ejective folds.
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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