释文：斜断层与褶皱轴向或区域构造线走向斜交的断层。
斜向断层是指断层走向与围岩走向斜交的断层。
An oblique fault is one that strikes obliquely or diagonally to the strike of the adjacent rocks.
推覆体侧缘发育了与边界断层平行的侧断坡、斜断坡次级断层相关褶皱背斜；
On the lateral border of the nappe, lateral and oblique fault-slope secondary fault-related folded anticlines parallel to boundary faults were developed.
背斜形态多为复式箱状背斜和不对称的斜歪背斜，分别与断层弯曲背斜和断层扩展背斜的几何形态一致。
The major morphology of the anticline is multiple box-shaped or asymmetry inclined, mostly, and it is similar to that of fault-bend fold and fault-propagation fold.
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