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Se and Te Mineralization in Albitites and Prospects of the Metasomatites for Au, Salla-Kuolajarvi Belt, Northern Karelia

机译:卡累利阿北部Salla-Kuolajarvi带的方铁矿中Se和Te的矿化作用以及变质岩的前景

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摘要

On the basis of the complex of geological features, the eastern flank of the Salla-Pana-Kuolajarvi belt is a prospect structure for gold mineralization in the U-bearing albitites and related acid and mafic metasomatites. Visible tellurides and selenides, which are typical of gold deposits of the Fe-Co-Au-U group in the adjacent territory of Finland within the Salla-Pana-Kuolajarvi belt, were found in the Ozerny occurrence as a result of studies. Native gold is found in association with tellurides. Molybdenite from the occurrence has a high Re content up to 0.3%.
机译:基于复杂的地质特征,Salla-Pana-Kuolajarvi带的东侧是含铀的方铁矿及相关的酸和镁铁质交代岩中金矿成矿的远景结构。研究表明,在Ozerny事件中发现了可见的碲化物和硒化物,它们是芬兰相邻地区Salla-Pana-Kuolajarvi带中Fe-Co-Au-U集团的金矿床的典型特征。发现天然金与碲化物有关。产生的辉钼矿的Re含量高达0.3%。

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    《Doklady Earth Sciences》 |2014年第1期|229-232|共4页
  • 作者单位

    Geological Institute, Kola Scientific Center, Russian Academy of Sciences, ul. Fersmana 14, Apatity, Murmansk oblast, 184209 Russia;

    Geological Institute, Kola Scientific Center, Russian Academy of Sciences, ul. Fersmana 14, Apatity, Murmansk oblast, 184209 Russia;

    Geological Institute, Kola Scientific Center, Russian Academy of Sciences, ul. Fersmana 14, Apatity, Murmansk oblast, 184209 Russia;

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