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五十年代,栖霞山矿区只是一个小型氧化锰矿床,经过多年的找矿勘探,现已探明为一个大型铅锌锰硫多金属矿床. 关于矿床的成因,曾有岩浆中-低温热液、沉积改造、火山热液成矿等观点.通过近年的地质研究,笔者认为,该矿床具有多源层控的特征,铅锌和锰的主要物源不同,矿体定位受层位和构造的控制.锰为同源层控,成矿物质主要来自石炭系碳酸盐地层;铅锌属异源层控,成矿物质主要来自前寒武系基底岩层.矿床的形成受地层
In the 1950s, the Qixiashan mining area was only a small type of manganese oxide deposit, and after many years of prospecting and exploration, it has been proved to be a large Pb-Zn-Mn-S polymetallic deposit.On the genesis of the deposit, there were medium-low temperature hydrothermal fluids, Depositional alteration and volcanic hydrothermal mineralization.According to recent geological studies, the author believes that this deposit has the characteristics of multi-source stratification control, the main source of lead, zinc and manganese are different, and the orebody location is controlled by horizon and structure Manganese is controlled by homologous strata, and the metallogenic materials are mainly derived from Carboniferous carbonate strata. Lead-zinc heterogeneous strata control and metallogenic materials are mainly from Precambrian basement strata.