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黄山岭铅锌矿经历了30多年开采历史,是一座资源枯竭型矿山,亟需探寻后备资源,而伴随着黄山岭以北新发现的桂林郑钼矿,有必要重新对矿床成因及控矿因素进行探讨,为下一步黄山岭矿区危机矿山找矿提供地质依据。矿区大地构造位置位于扬子准地台沿江拱断褶带的安庆凹断束。次级构造单元位于七都复背斜之大佛堂-太平曹背斜中段-黄山岭背斜南东翼(如图1)。矿区主要出露地层为奥陶系下统的仑山组至志
Huangshanling lead-zinc mine experienced more than 30 years of mining history, is a resource-depleted mine, urgent need to explore the reserve resources, and along with Huangshan Ridge newly discovered Guilin Zheng molybdenum mine, it is necessary to re-deposit genesis and ore-controlling factors Explore, provide the geological basis for prospecting for the crisis mine in Huangshanling mining area in the next step. The tectonic location of the mining area is located at the Anqing Concave Beam of the arch fold along the Yangtze River. The secondary structural units are located in the middle of the Taiping Cao anticline, the large east-west wing of the Huangshanling anticline, as shown in Figure 1. The main exposed strata in the mining area are Zhoushan Group of Lunshan Formation under the Ordovician