本文从边界构造、滑动形态特征与力学性质、滑动系统、下伏系统、运动方向等方面 ,系统地分析研究了新密大平—超化滑动构造的总体特征。新密大平—超化滑动构造南北以背斜为界 ,东西受断层切割 ;滑面具有穿层现象且次级滑面发育 ;其力学性质为压扭性 ,南翼还兼有张性 ;滑动系统总体表现为向斜构造 ;滑动方向晚期呈现出先南后北的特征。 In this paper, we systematically analyze and study the general features of the Daping-Chaohua slip tectonics in the Xinmi Formation from the aspects of boundary structure, sliding morphology and mechanical properties, sliding system, underlying system and moving direction. Xinmi Daping - super-migratory structure North-South anticline as the boundary, something cut by the fault; the slip surface with the phenomenon of stratification and the secondary slide surface development; its mechanical properties of compression and torsion, the south wing also has tension; sliding The system is generally characterized by an anticline structure; the slipping direction exhibits the characteristics of south-north-south-north.