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文章结合前人的资料,通过矿区开展的基础地质勘查和取样化验分析,对银升坪重晶石矿的区域地质和矿床地质特征及成因进行了分析研究,初步认为该重晶石矿床受断裂控制,是后期热液充填于次一级断和裂隙中生成的产物,属单金属硫化物-重晶石矿类型。该区范围具有找矿前景,根据矿脉赋存、分布规律和成矿特点,提出了以矿点为中心向外围找矿的设想。
Based on the previous data and through the basic geological survey and sampling and laboratory analysis carried out in the mining area, this paper analyzes the regional geology and geological characteristics and genesis of the Yinshengping barite deposit, and initially concludes that the barite deposit is subject to fracture Control, is the late hydrothermal filling in the secondary fault and fracture products generated, is a single metal sulfide - barite type. According to the occurrence, distribution and ore-forming characteristics of the veins, the idea of prospecting out to the periphery with the mine point as the center is proposed.