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Magmatities of the Ebe-Khaya Dike Belt as a Possible Primary Source of Placer Diamonds in the Northeastern Part of the Siberian Platform

机译:Ebe-Khaya堤防带的巨变可能是西伯利亚平台东北部砂岩的主要来源

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摘要

Along the periphery of ancient platforms (Africa, South America, Australia), some large alluvial diamond placer deposits with unknown primary sources of their origin are located [1, 2]. A similar situation is observed in the northeastern part of the Siberian platform in the Anabar River basin, where together with numerous nondiamond and diamond-poor kimberlite bodies there are Ebelyakh placers, unique in the resources and quality of diamonds [3, 4].
机译:在古代平台的外围(非洲,南美,澳大利亚),发现了一些大型冲积砂金矿床,其来源不明[1,2]。在阿纳巴尔河流域的西伯利亚台地东北部也观察到了类似的情况,那里有许多无钻石和贫金刚石的金伯利岩体,还有埃比利亚克砂矿,在钻石的资源和质量上是独一无二的[3,4]。

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  • 来源
    《Doklady Earth Sciences》 |2010年第1期|p.285-287|共3页
  • 作者

    M. D. Tomshin;

  • 作者单位

    Institute of the Geology of Diamonds and Noble Metals, Siberian Branch, Russian Academy of Sciences, pr. Lenina 39, Yakutsk, 678980 Russia;

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  • 正文语种 eng
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  • 入库时间 2022-08-18 03:38:03

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