武夷山元古界沉积-变质型铅锌矿成矿地质特征

On the Geological Mineralization Features of a Sedimentary Metamorphic Typed Lead-zinc Mine in Wuyi Mountain

  • 摘要: 位于武夷山成矿带中的江西铅山观星岭铅锌矿,以及福建建瓯八外洋、溪源、峰岩、水吉等铅锌矿成矿特征相似;矿(化)体的形成先后与矿源层、变质热液、岩浆热液改造有着密切的成因联系.受层位和岩性控矿相当明显,具有同生型层控矿床的基本特征.

     

    Abstract: Guangxinling Lead-zinc ore, which locates in Wuyi Mountain mineralization belt, resembles in terms of its mineralization features to the neighbouring Lead-zinc mine in Fujian province. The formation of ore body is closely associated with ore source bed, metamorphic hydrothermal and magma hydrothermal transformation. The ore has the basic features of syngenetic strata-bound deposit.

     

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