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    尉向东, 郭文秀. 豫西地区金矿的氧、铅、碳同位素特征与成矿流体[J]. 地质与资源, 1997, 6(2): 114-123.
    引用本文: 尉向东, 郭文秀. 豫西地区金矿的氧、铅、碳同位素特征与成矿流体[J]. 地质与资源, 1997, 6(2): 114-123.
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    Yu Xiangdong, Guo Wenxiu. OXYGEN, LEAD AND CARBON ISOTOPIC CHARACTERISTICS AND ORE-FORMING FLUIDS OF GOLD DEPOSITS IN WEASTERN HENAN[J]. Geology and Resources, 1997, 6(2): 114-123.
    Citation: Yu Xiangdong, Guo Wenxiu. OXYGEN, LEAD AND CARBON ISOTOPIC CHARACTERISTICS AND ORE-FORMING FLUIDS OF GOLD DEPOSITS IN WEASTERN HENAN[J]. Geology and Resources, 1997, 6(2): 114-123.
    shu

    豫西地区金矿的氧、铅、碳同位素特征与成矿流体

    OXYGEN, LEAD AND CARBON ISOTOPIC CHARACTERISTICS AND ORE-FORMING FLUIDS OF GOLD DEPOSITS IN WEASTERN HENAN

      摘要
    • 摘要: 通过对豫西众多金矿床的氧、铅、碳同位素的研究,认为豫西金矿的成矿流体是一种在长期地质演化过程中形成的广泛均一化的深部地壳流体。成矿作用乃是深部流体由下向上运移与由上向下渗透的大气降水相遇、混合,从而引起流体物化条件快速变化,导致金等成矿物质沉淀。

       

      Abstract: On the basis of O, Pb and C isotopic studies of many gold deposits in western Henan, The authors suggest that the ore-forming fluid of gold deposits is deep flow. It was formed at great depths during evolution of geology. Mineralization was related to the fluids that flowed from deep to upper and was hybridized by meteoric water.

       

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