许映邦. 1985: 水系重砂矿物含量浅析. 地质通报, (5): 121-127.
    引用本文: 许映邦. 1985: 水系重砂矿物含量浅析. 地质通报, (5): 121-127.
    XU Ying-bang. 1985: HEAVY MINERAL CONTENT IN A DRAINAGE SYSTEM. Geological Bulletin of China, (5): 121-127.
    Citation: XU Ying-bang. 1985: HEAVY MINERAL CONTENT IN A DRAINAGE SYSTEM. Geological Bulletin of China, (5): 121-127.

    水系重砂矿物含量浅析

    HEAVY MINERAL CONTENT IN A DRAINAGE SYSTEM

    • 摘要: 一、前言水系重砂测量是区调工作中常用找矿手段之一。对于重砂矿物含量的认识与处理方法为: (一)普遍认为水系重砂矿物含量高,异常区级别就高,找矿意义就大。反之则低则小。因而,普遍以水系重砂矿物含量级别与异常区级别相吻合或相当为特征。 (二)水系重砂矿物含量级别划分不统一。同种重砂矿物的含量,划成三、四、五个级别的均有。 (三)大多数单位用统计法求重砂矿物含量背景值,划分含量级别。少数单位用数据处理方法整理和解释区域水系重砂矿物含量资料。并谓为“它所带来的优越性与我们比较熟

       

      Abstract: The heavy mineral content in a drainage system involves a superficial quantity concept formed by the combined effect of a series of internal and external factors. Its prime significance is to provide a mineral basis for finding target areas.However, only through conducting a concrete comprehen- sive study, revealing its nature and recognizing its attribute, can its significance in quantity be judged and can it be used as a parameter for determining the order of an anomalous area. It shows not only symmetry to the primary (or secondary) source but also nonsymmetry. In the past stress was put on symmetry, while nonsymmetry was neglected;as a result, anomalies were missing. In this case, the significance of an anomalous area in mineral prospecting was artificially raised and reduced. Its nature calls for a corresponding improvement of the full sequence of present placer mineral prespecting in a drainage system.

       

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