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首页> 外文期刊>Doklady Earth Sciences >Paleozoic U-Pb Age of Rutile Inclusions in Diamonds of the V-VII Variety from Placers of the Northeast Siberian Platform
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Paleozoic U-Pb Age of Rutile Inclusions in Diamonds of the V-VII Variety from Placers of the Northeast Siberian Platform

机译:来自东北西伯利亚平台矿床的V-VII品种钻石中的金红石夹杂物的古生代U-Pb年龄

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摘要

Diamonds attributed according to the classification of Yu.L. Orlov to the Vand VII varieties are widespread in rich placers of the northeastern part of the Siberian Platform [6]. Mineralogical investigation (certification) of these diamonds showed that they represent a unified genetical type subdivided by Orlov according to the following formal characteristics: diamonds of the V variety are represented by monocrys-tals, and diamonds of the VII variety are represented by intergrowths. Thus, we unite them into one variety V-VII [2].
机译:根据Yu.L.范德七世的奥尔洛夫广泛分布在西伯利亚台地东北部的富砂矿中[6]。这些钻石的矿物学研究(证明)表明,它们代表着Orlov根据以下正式特征细分的统一遗传类型:V型钻石由单晶代表,而VII型钻石则由共生代表。因此,我们将它们组合成一个V-VII品种[2]。

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  • 来源
    《Doklady Earth Sciences》 |2009年第7期|1151-1155|共5页
  • 作者单位

    Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Koptvuga pr. 3, Novosibirsk 90, 630090 Russia;

    Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Koptvuga pr. 3, Novosibirsk 90, 630090 Russia;

    Earthquake Research Institute, The University of Tokyo, Yayoil 1-1-1, Bunkyo-ku, Tokyo, 113-0032, Japan;

    Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Koptvuga pr. 3, Novosibirsk 90, 630090 Russia;

    Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Koptvuga pr. 3, Novosibirsk 90, 630090 Russia;

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