文美兰, 欧阳菲. 2013: 广西平桂地区锡矿土壤离子电导率异常特征和离子成分及找矿预测. 地质通报, 32(5): 784-789.
    引用本文: 文美兰, 欧阳菲. 2013: 广西平桂地区锡矿土壤离子电导率异常特征和离子成分及找矿预测. 地质通报, 32(5): 784-789.
    WEN Mei-lan, OUYANG Fei. 2013: Anomaly characteristics, components of soil ionic conductivity and prospecting prediction of tin deposits in Pinggui area, Guangxi. Geological Bulletin of China, 32(5): 784-789.
    Citation: WEN Mei-lan, OUYANG Fei. 2013: Anomaly characteristics, components of soil ionic conductivity and prospecting prediction of tin deposits in Pinggui area, Guangxi. Geological Bulletin of China, 32(5): 784-789.

    广西平桂地区锡矿土壤离子电导率异常特征和离子成分及找矿预测

    Anomaly characteristics, components of soil ionic conductivity and prospecting prediction of tin deposits in Pinggui area, Guangxi

    • 摘要: 为了解广西平桂地区锡矿土壤离子电导率异常特征,研究不同种类离子的含量变化关系对电导率的贡献大小,为解释锡矿土壤离子电导率异常的形成机制提供理论依据。对广西平桂地区锡矿的土壤离子电导率异常进行研究,结果表明:①在已知锡矿体上测出了清晰的土壤离子电导率异常,异常形态呈典型双峰形态“兔耳”状或“单峰”状, 异常垂直指示锡矿体的赋存位置;②弄清了锡矿体组成土壤离子电导率异常的离子成分特征,其成分主要是SO42-、Ca2+、HCO3-、Cl-、Fe3+、Mg2+、Na+、K+、Mn2+、F-等一套水可溶性离子,经过相关分析得出锡矿土壤离子电导率异常与各种水可溶性离子的相关系数SO42->Ca2+>HCO3->Cl->Fe3+>Mg2+>Na+>K+>Mn2+>F-;③在未知区的找矿预测中找到2个具有成矿远景的土壤离子电导率异常,经深部工程验证找到了隐伏锡矿体。

       

      Abstract: Although the conventional geochemical methods are thought better effect methods which are used to prospect and explore in the all kinds of coverage area, it is not clear what their most effective role is in prospecting in the Karst residual slope laminated coverage area Pinggui area in Guangxi province. This research is mainly concerned with a study of anomaly characteristics of soil ionic conductivity on tin deposits in Pinggui area in Guangxi Province. The investigation to test the validity of prospecting in the approach was carried out above the known ore bodies revealed that the clear soil ionic conductivity anomalies are detected over ore bodies,and which appeared two typical summits resembling shapes which are look like a "rabbit ear" or "hard iron teeth". Further research needs to be conducted to determine by experiment that the main water soluble ions which make up the anomaly of soil ionic conductivity of tin deposits are including SO42-, Ca2+, HCO3-, Cl-, Fe3+, Mg2+, Na+, K+, Mn2+ and F- , and their relation degree between the tin anomaly are as follow: SO42->Ca2+>HCO3->Cl->Fe3+>Mg2+>Na+>K+>Mn2+>F-.This fruitful work provided theory basis to explain soil ionic conductivity anomaly. On the basis of it , we finally carried out prospecting prediction by this method in the area and found two predictive targets where five ore bodies were found by the engineering drill.

       

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