Faults are vertically subdivided into deep fault system and shallow fault system by the bottom of Jurassic Formation at Wuxia area.
根据地震解释结果，本区断裂系统在纵向上具有明显的分层性，以侏罗系底为界，划分为深部和浅部两套断裂系统。
Deep and shallow fault system have succession with time and space in the south of the work area, to the north have their own structural causes and the corresponding sub-detachment surfaces.
深、浅断裂体系在工区南部具有时间与空间上的继承性，往北深、浅断裂体系具有独自的构造成因和对应的次级滑脱面。
The key structure in this area is a duplex that comprises of a shallow fault-bend fold of the Late Triassic and a deep blind stacking anticline imbricated by three thrust sheets of Cenozoic age.
矿山梁构造几何学上表现为一个双重构造：浅层是一个晚三叠世形成的断层转折褶皱；深层则是在新生代形成的三个逆冲岩片叠置所构成的隐伏堆垛背斜构造。
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