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发育于矿区下二叠统的同沉积断层,伴有一系列海底热水沉积成矿的迹象和滑塌堆积及浊流沉积、变基性熔岩等,致使含矿地层局部出现厚度的剧变,并造成各区段不同的成矿特点。对区域及矿区一些地质现象的解释和内部规律的研究具有重要意义。
Developed in the lower Permian synsedimentary fault, with a series of signs of seafloor hydrothermal sedimentary mineralization and slump accumulation and turbidity flow deposition, metamorphic lava, etc., resulting in local changes in the thickness of the ore-bearing strata and caused Different sections of the metallogenic characteristics. It is of great significance to study the interpretation and internal laws of some geological phenomena in the area and the mining area.