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湘潭锰矿是一个有七十三年历史的老矿山,现在已发展成为有采、选、烧、冶的联合企业,是我国重要锰业基地之一。湘潭锰矿矿床为浅海沉积碳酸锰矿床,位于江南古陆南缘的中部,区域构造位置属于伯女山背斜北翼之中部,自东向西依次为冷水冲连续褶皱带,青山、黄峰寺和石冲单斜带。矿体赋存于震旦系炭质黑色页岩中,顶板岩层为
Xiangtan manganese ore is a 73-year-old mines and has now developed into a coal mining, election, burning, metallurgical joint venture, is one of China’s major manganese industry base. The Xiangtan manganese ore deposit is a shallow-sea sedimentary carbonate-manganese deposit located in the middle of the southern margin of the southern South China Plain. The regional tectonic belonged to the central part of the north wing of the Boye Mountain anticline, followed by the Lengshuian continuous fold belt from east to west, and the Qingshan, Huangfeng Temple and Shi Chong Single oblique belt. Ore bodies occur in the Sinian carbonaceous black shale, roof rock formation