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First Occurrences of Terrigenic Gold and Platinum in the Miocene Sediments of the Eastern Caucasus, Dagestan

机译:达吉斯坦东部高加索地区的中新世沉积物中首次发生致源性金和铂

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摘要

There are no magmatic formations in the Eastern Caucasus that could be sources of primary ore or placer occurrences of gold and platinum. That is why geological works for these metals are practically absent. Gold and silver were determined as a by-product during geological exploration works at the pyritic and quartz-sul-fide vein ores as well as during geological surveying (Sevkavgeologiya). Occurrences of the enriched concentrations of Au, Pt, and Pd in the Miocene sandy-argillaceous sediments located in the amagmatic territory at the conjugation between the northern slope of the Eastern Caucasus orogene and Tersk-Kaspian fore-deep were not predicted.
机译:东高加索地区没有岩浆形成可能是金和铂的原矿或砂矿出现的来源。这就是为什么实际上没有这些金属的地质作用的原因。在黄铁矿和石英硫化矿脉矿石的地质勘探工作中以及在地质勘测期间(Sevkavgeologiya),黄金和白银都是副产品。预测东高加索造山带北坡与特尔斯克-卡斯皮亚前缘深部接合处位于中冰期的中新世沙质-泥质沉积物中金,铂和钯的富集不会发生。

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  • 来源
    《Doklady Earth Sciences》 |2009年第2期|223-225|共3页
  • 作者单位

    Institute of Geology, Dagestan Scientific Center,Russian Academy of Sciences, Makhachkala,ul. M. Yaragskogo 75, 367030 Dagestan Republic, Russia;

    Institute of Geology, Dagestan Scientific Center,Russian Academy of Sciences, Makhachkala,ul. M. Yaragskogo 75, 367030 Dagestan Republic, Russia;

    Institute of Geology, Dagestan Scientific Center,Russian Academy of Sciences, Makhachkala,ul. M. Yaragskogo 75, 367030 Dagestan Republic, Russia;

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