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浙江武义萤石矿田中金（银）－萤石矿床，是中国首次发现并厘定的元素地球化学性质迥异，但物源、力源又相同，受同构造控制，形成于同一成矿期不同成矿阶段的金（银）－萤石矿床新类型。矿床严格受控于盆地构造格局的时空演化规律和帚状控矿构造型式，对中国东部中生代火山岩带萤石矿田（床）中金（银）矿的寻找具有极为重要的实践和理论价值。
The gold (silver) -fluorite deposit in Wuyi fluorite orefield in Zhejiang is the first element discovered and determined by China to have very different geochemical characteristics. However, the source and source of the same are controlled by the same tectonics and formed at the same stage of mineralization Gold (silver) - a new type of fluorite deposit in the mine. The deposit is strictly controlled by the spatial and temporal evolution of the structural pattern of the basin and the broom-like ore-controlling structural pattern, which is of extremely important practical and theoretical value in the search for the gold (silver) deposits in the fluorite orefield (bed) of the Mesozoic volcanic belt in eastern China.