罗镇宽, 关康. 河南祁雨沟金矿床地质地球化学特征和矿床成因讨论[J]. 地质与资源, 1995, 4(1): 1-12.
    引用本文: 罗镇宽, 关康. 河南祁雨沟金矿床地质地球化学特征和矿床成因讨论[J]. 地质与资源, 1995, 4(1): 1-12.
    Luo Zhenkuan, Guan Kang. GEOLOGY AND GEOCHEMICAL FEATURES OF QIYUGOU GOLD DEPOSIT IN HENAN PROVINCE AND DISCUSSIONS ON THE GENESIS OF ORE DEPOSIT[J]. Geology and Resources, 1995, 4(1): 1-12.
    Citation: Luo Zhenkuan, Guan Kang. GEOLOGY AND GEOCHEMICAL FEATURES OF QIYUGOU GOLD DEPOSIT IN HENAN PROVINCE AND DISCUSSIONS ON THE GENESIS OF ORE DEPOSIT[J]. Geology and Resources, 1995, 4(1): 1-12.

    河南祁雨沟金矿床地质地球化学特征和矿床成因讨论

    GEOLOGY AND GEOCHEMICAL FEATURES OF QIYUGOU GOLD DEPOSIT IN HENAN PROVINCE AND DISCUSSIONS ON THE GENESIS OF ORE DEPOSIT

    • 摘要: 本文介绍了祁雨沟金矿床的成矿地质背景和矿床地质地球化学特征,讨论了矿床成因。通过含矿角砾岩体特征、矿物学、硫、铅、氢、氧同位素地质学和流体包裹体的研究,确定成矿物质主要来自下伏太古宇太华群;气液爆破角砾岩体为容矿构造;成矿作用是在中生代岩浆活动期后气液爆破-沸腾作用下完成的;成矿流体以岩浆水为主,混入部分大气水;矿床成因属岩浆热液矿床。

       

      Abstract: In this paper, the authors has introduced the geological background of mineralization and geology and geochemical features of Qiyugou gold deposit, discussed the genesis of ore de-posit.Through the research on the feature of rock body mineralogy, S, Pb, H and O isotopic geology and fluid inclusion of the ore-bearing breccia body, the authors conside that the ore-forming material mainly came from the underlying Taihua Group of Archean eonothem. Gas-liquid explosive breccia body is the host structure.Mineralization went on under the condition of gas-liquid explosion-boiling action after Mesozoic magmatic activity stage. Mineralizing fluid is mainly magmatic water, and mixed with part of meteorological water.The genesis of ore deposit belong to magmatic hydrothermal deposit.

       

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