该推覆体由数条撕裂断层分为几个叠瓦体，各有不同的形态、结构特征。
This nappe group is divided into several imbricates by several tear faults, each of which has different features with respect to its shape and structure.
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。
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.
在叠后地震资料处理中，断层保护是十分重要的。
Faults protecting is very important during post stack seismic data processing.
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