严己宽. 2011: “区域异常集中度”的概念、计算方法及其与成矿的关系. 地质通报, 30(11): 1802-1808.
    引用本文: 严己宽. 2011: “区域异常集中度”的概念、计算方法及其与成矿的关系. 地质通报, 30(11): 1802-1808.
    YAN Ji-kuan. 2011: The concept and calculation method of “the concentration ratio of regional geochemical anomaly” and the relationship between it and the ore-forming. Geological Bulletin of China, 30(11): 1802-1808.
    Citation: YAN Ji-kuan. 2011: The concept and calculation method of “the concentration ratio of regional geochemical anomaly” and the relationship between it and the ore-forming. Geological Bulletin of China, 30(11): 1802-1808.

    “区域异常集中度”的概念、计算方法及其与成矿的关系

    The concept and calculation method of “the concentration ratio of regional geochemical anomaly” and the relationship between it and the ore-forming

    • 摘要: 为了解释普遍存在的成矿规模与区域化探异常面积大小不成比例的问题,提出了“区域异常集中度”的概念,给出了概念的定义、相关要素和计算方法。探讨了区域异常集中度的主要特点,数值大小、计算尺度与成矿规模的关系,适用条件等。认为区域异常集中度反映了成矿物质的集中程度,应用它找大矿是在区域成矿要素范围内众多异常中“同中求异”的过程。初步提出了区域成矿要素集中度的概念,并讨论了它与区域异常集中度的关系。区域异常集中度的提出为区域化探异常解释评价提供了一个全新的地质地球化学指标和视角,将成矿相关元素异常与区域成矿要素联系起来的综合方法对于深化异常与成矿关系的认识有重要意义,对于寻找大中型矿床或矿田有重要的指导作用。

       

      Abstract: Aimed at solving the commonly-existent problem that the ore-forming scale is not in proportion to the area of regional geochemical anomaly, this paper puts forward a new concept of “the concentration ratio of regional geochemical anomaly”, describes its definition, related elements and method of calculation. Its main features and adaptability conditions as well as the relationship between the value and scale of the concentration ratio of regional geochemical anomaly and the mineralization size are also discussed. It is held that the concentration ratio of regional geochemical anomaly is a mirror of the concentration ratio of regional ore-forming materials. With this new concept, we can find large-size ore deposits by looking for regional geochemical anomalies. This paper advances a new concept of the intensity of regional ore-forming geological essential factors, and investigates the relationship between the concentration ratio of regional geochemical anomaly and the intensity of regional mineralization geological essential factors.

       

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