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Rhenium Distribution in Molybdenite: Results of Microprobe Scanning (Copper Porphyry Deposits, the Urals)

机译:钼矿中的分布:显微探针扫描的结果(铜斑岩矿床,乌拉尔)

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摘要

The geochemistry of rhenium in ores of copper porphyry deposits from various regions has been considered in numerous papers presented in the reviews [1-3 and others]. We have recently systematized analyses for the Urals [4]. Estimations of this element in different parts of separate molybdenite grains are very scarce [3,5,6, and others]. Data on rhenium scanning in molybdenite grains are not available. However, the pattern of rhenium distribution in molybdenite grains is very important for understanding of the conditions of its precipitation and further redistribution within deposits especially those that have undergone low-temperature modifications and deformations.
机译:评论[1-3等]中发表的许多论文都考虑了来自不同地区的铜斑岩矿床中矿石中ium的地球化学。我们最近对乌拉尔[4]进行了系统化分析。在单独的辉钼矿颗粒的不同部分中对该元素的估计非常稀缺[3、5、6等]。无法获得有关辉钼矿晶粒中scanning扫描的数据。但是,mo在辉钼矿晶粒中的分布方式对于理解其沉淀条件以及进一步沉积在沉积物中的再分布非常重要,尤其是经历了低温改性和变形的沉积物。

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  • 来源
    《Doklady Earth Sciences》 |2010年第1期|p.351-355|共5页
  • 作者单位

    Zavaritskii Institute of Geology and Geochemistry, Ural Division, Russian Academy of Sciences, Yekaterinburg, Russia;

    Zavaritskii Institute of Geology and Geochemistry, Ural Division, Russian Academy of Sciences, Yekaterinburg, Russia;

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