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铜鼓山铅锌矿位于扬子准地台西缘,康滇地轴东沿,三江成矿带北段。区内地层除泥盆系、石炭系缺失外,其余自震旦系至白垩系均有出露。其中震旦系上统灯影组是区内铅锌矿的主要赋矿地层。经矿床地质特征研究认为,研究区矿体连续性较好,矿(化)体有由地表至深部有变富变厚的趋势,在有利的成矿环境下易形成富大的矿(化)体。本区有值得进一步地质工作或初步具有开发利用铅锌矿山的价值。
Tonggu Mountain lead-zinc mine is located in the western margin of the Yangtze Platform, Kang Dian axis east along the northern section of the Sanjiang metallogenic belt. In addition to the Devonian and Carboniferous, the rest of the strata are exposed from the Sinian to the Cretaceous. The Upper Sinian Dengying Formation is the main ore-bearing formation of lead-zinc deposits in the area. According to the geological characteristics of the deposit, the continuity of the ore body in the study area is good. The ore body has the tendency of getting rich and thickening from the surface to the deep. It is easy to form rich ore (ore) body. The area is worth further geological work or initial development and utilization of the value of lead-zinc mines.