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以构造层次的观点剖析了乌拉山塑性变形构造、韧性剪切带和脆性断裂构造的特征及其演化，认为东西向浅层次的脆性断裂——山前大断裂是乌拉山金矿的导矿构造，其后期（加里东—海西）活动派生的近东西向呈右行雁列的一组剪切断裂是容矿构造，并认为容矿断裂是经历了先压后张２个阶段的脆性断裂。
Analyze the characteristics and evolution of the plastic deformation structure, ductile shear zone and brittle fracture structure in Wula Mountain from the structural level, and consider the shallow brittle faults in the east-west direction - the great piedmont fault is the guide mineral of the Wulashan gold deposit A series of shear faults derived from the near east-west geese derived from the later (Caledonian-Hercynian) activity are the ore-hosting structures. It is considered that the ore-hosting faults experienced brittleness in the first two stages of post-tensioning and post-tensioning fracture.