大池干井构造带是川东高陡构造带之一。
The Dachigan structural zone is one of the steep structural zones in Eastern Sichuan Basin.
大池干井构造带的形成不仅在石炭系内形成了众多的裂缝，而且使背斜核部的孔隙度增高。
The formation of Dachigan steep structural zone not only generates many fissures in Upper Carboniferous, but also makes the porosity of Upper Carboniferous higher in the core of these anticlines.
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