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    刘显凡, 朱赖民, 金景福, 倪师军. 微细浸染型金矿常量元素地球化学特征与深部物质来源示踪——以滇黔桂三角区金矿为例[J]. 地质与资源, 1998, 7(1): 48-57. DOI: 10.13686/j.cnki.dzyzy.1998.01.005
    引用本文: 刘显凡, 朱赖民, 金景福, 倪师军. 微细浸染型金矿常量元素地球化学特征与深部物质来源示踪——以滇黔桂三角区金矿为例[J]. 地质与资源, 1998, 7(1): 48-57. DOI: 10.13686/j.cnki.dzyzy.1998.01.005
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    Liu Xianfan, Zhu Laimin, Jin Jingfu, Ni Shijun. GEOCHEMISTRY OF COMMON ELEMENT AND PLUTONIC MATERIAL ORIGINATING TRACE FOR CARLINTYPE GOLD DEPOSITS-A CASE STUDY OF THE GOLD DEPOSITS IN YUNNANGUIZHOUGUANGXI TRIANGLE AREA[J]. Geology and Resources, 1998, 7(1): 48-57. DOI: 10.13686/j.cnki.dzyzy.1998.01.005
    Citation: Liu Xianfan, Zhu Laimin, Jin Jingfu, Ni Shijun. GEOCHEMISTRY OF COMMON ELEMENT AND PLUTONIC MATERIAL ORIGINATING TRACE FOR CARLINTYPE GOLD DEPOSITS-A CASE STUDY OF THE GOLD DEPOSITS IN YUNNANGUIZHOUGUANGXI TRIANGLE AREA[J]. Geology and Resources, 1998, 7(1): 48-57. DOI: 10.13686/j.cnki.dzyzy.1998.01.005
    shu

    微细浸染型金矿常量元素地球化学特征与深部物质来源示踪——以滇黔桂三角区金矿为例

    GEOCHEMISTRY OF COMMON ELEMENT AND PLUTONIC MATERIAL ORIGINATING TRACE FOR CARLINTYPE GOLD DEPOSITS-A CASE STUDY OF THE GOLD DEPOSITS IN YUNNANGUIZHOUGUANGXI TRIANGLE AREA

      摘要
    • 摘要: 通过主要常量元素数据的多元统计分析，探讨了该区金矿的地球化学演化规律，论证了成矿物质主要直接来源于上地慢分异，从而较圆满地解释了成矿物质既来源于深部，但又与地壳（地层）物质有密切关联的独特地质地球化学特征.

       

      Abstract: Based on the multivariate correlation statistical analysis of main common element data,this paper discusses the evolution law of geochemistry for the gold deposits in the studied area,proves that ore materials may be directly derived from upper mantle differentiation mainly,and satisfactorily explains the typical geology-geochemistry nature that the ore materials are from upper mantle but in association with crust (strata) matter.

       

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