Abstract
The composition of volatiles from fluid and melt inclusions in olivine phenocrysts from Yakutian kimberlite pipes of various ages (Olivinovaya, Malokuonapskaya, and Udachnaya-East) were studied for the first time by gas chromatography–mass spectrometry. It was shown that hydrocarbons and their derivatives, as well as nitrogen-, halogen-, and sulfur-bearing compounds, played a significant role in the mineral formation. The proportion of hydrocarbons and their derivatives in the composition of mantle fluids could reach 99%, including up to 4.9% of chlorineand fluorine-bearing compounds.
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Original Russian Text © A.A. Tomilenko, T.A. Bul’bak, M.O. Khomenko, D.V. Kuzmin, N.V. Sobolev, 2016, published in Doklady Akademii Nauk, 2016, Vol. 468, No. 6, pp. 684–689.
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Tomilenko, A.A., Bul’bak, T.A., Khomenko, M.O. et al. The composition of volatile components in olivines from Yakutian kimberlites of various ages: Evidence from gas chromatography–mass spectrometry. Dokl. Earth Sc. 468, 626–631 (2016). https://doi.org/10.1134/S1028334X16060234
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DOI: https://doi.org/10.1134/S1028334X16060234