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首页> 外文期刊>Doklady Earth Sciences >Peculiarities of the Composition of Zoned Picroilmenites from the Massadou Field (Giunea) and Dachnaya Pipe (Yakutia) Kimberlites
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Peculiarities of the Composition of Zoned Picroilmenites from the Massadou Field (Giunea) and Dachnaya Pipe (Yakutia) Kimberlites

机译:Massadou田地(Giunea)和Dachnaya Pipe(雅库特)金伯利岩的带状紫云母组成的特殊性

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摘要

Numerous publications [1, 3, 6, 11, 12, 14] concern picroilmenite, a magnesium variety of ilmenite typical for kimberlite. This mineral attracts interest in light of the kimberlite petrogenesis, as well as because it is the most abundant kimberlite indicator. In some cases the concentration of picroilmenite in kimberlite is tens kg/t [2], and the grain sizes range from 0.0n mm to 15 cm. Picroilmenite is quite abundant in xenoliths of garnet lherzolite including cataclastic ones and wehrlite [3, 5].
机译:许多出版物[1、3、6、11、12、14]都提到了云母钛铁矿,这是金伯利岩中典型的镁钛铁矿。鉴于金伯利岩的岩石成因,以及由于它是最丰富的金伯利岩指示剂,这种矿物引起了人们的兴趣。在某些情况下,金伯利岩中的次青铁矿浓度为数十kg / t [2],晶粒尺寸为0.0n mm至15 cm。石榴石锂铁矿的异岩中的次硅铁石含量非常丰富,包括碎屑岩和辉绿岩[3,5]。

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  • 来源
    《Doklady Earth Sciences》 |2010年第2期|p.1386-1389|共4页
  • 作者单位

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

    rnSobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, pr. Akad. Koptyuga 3, Novosibirsk, 630090 Russia;

    rnSobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, pr. Akad. Koptyuga 3, Novosibirsk, 630090 Russia;

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