武夷山元古界沉积-变质型铅锌矿成矿地质特征

来源期刊：有色金属科学与工程2010年第1期

论文作者：王显华

文章页码：85 - 90

关键词：矿源层；变质热液；岩浆热液改造；多旋回性；多阶段性

Key words：ore source bed; metamorphic hydrothermal; magma hydrothermal transformation; multi-cyclicity; multi-phase

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.