The Wenan Slope was characterized by the structure of "deep channel and high horst", while the Yangcun Slope showed a relative simple monoclinic.
杨村斜坡不具有相邻文安斜坡“深沟高垒”式的垒嵌结构，而是一个相对简单的单斜。
The structural style found in the basin includes imbricated thrust zone, trapdoor structure, drag fold, listric fault, rollover anticline, horst-graben structure and the like.
盆地中发育多种构造样式，主要有：叠瓦状冲断层、滚板构造、牵引褶皱、铲形正断层、滚动背斜、“垒一堑”构造等。
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