The composition of volatile components in olivines from Yakutian kimberlites of various ages: Evidence from gas chromatography–mass spectrometry

A. A. Tomilenko, T. A. Bul’bak, M. O. Khomenko, D. V. Kuzmin, N. V. Sobolev

Результат исследования: Научные публикации в периодических изданияхстатьярецензирование

12 Цитирования (Scopus)

Аннотация

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.

Язык оригиналаанглийский
Страницы (с-по)626-631
Число страниц6
ЖурналDoklady Earth Sciences
Том468
Номер выпуска2
DOI
СостояниеОпубликовано - 1 июн 2016

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