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The composition of volatile components in olivines from Yakutian kimberlites of various ages : Evidence from gas chromatography–mass spectrometry. / Tomilenko, A. A.; Bul’bak, T. A.; Khomenko, M. O. и др.

в: Doklady Earth Sciences, Том 468, № 2, 01.06.2016, стр. 626-631.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Tomilenko, AA, Bul’bak, TA, Khomenko, MO, Kuzmin, DV & Sobolev, NV 2016, 'The composition of volatile components in olivines from Yakutian kimberlites of various ages: Evidence from gas chromatography–mass spectrometry', Doklady Earth Sciences, Том. 468, № 2, стр. 626-631. https://doi.org/10.1134/S1028334X16060234

APA

Tomilenko, A. A., Bul’bak, T. A., Khomenko, M. O., Kuzmin, D. V., & Sobolev, N. V. (2016). The composition of volatile components in olivines from Yakutian kimberlites of various ages: Evidence from gas chromatography–mass spectrometry. Doklady Earth Sciences, 468(2), 626-631. https://doi.org/10.1134/S1028334X16060234

Vancouver

Tomilenko AA, Bul’bak TA, Khomenko MO, Kuzmin DV, Sobolev NV. The composition of volatile components in olivines from Yakutian kimberlites of various ages: Evidence from gas chromatography–mass spectrometry. Doklady Earth Sciences. 2016 июнь 1;468(2):626-631. doi: 10.1134/S1028334X16060234

Author

Tomilenko, A. A. ; Bul’bak, T. A. ; Khomenko, M. O. и др. / The composition of volatile components in olivines from Yakutian kimberlites of various ages : Evidence from gas chromatography–mass spectrometry. в: Doklady Earth Sciences. 2016 ; Том 468, № 2. стр. 626-631.

BibTeX

@article{ba7fbae5a50a41e0ba214e648f65bb57,
title = "The composition of volatile components in olivines from Yakutian kimberlites of various ages: Evidence from gas chromatography–mass spectrometry",
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.",
author = "Tomilenko, {A. A.} and Bul{\textquoteright}bak, {T. A.} and Khomenko, {M. O.} and Kuzmin, {D. V.} and Sobolev, {N. V.}",
year = "2016",
month = jun,
day = "1",
doi = "10.1134/S1028334X16060234",
language = "English",
volume = "468",
pages = "626--631",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - The composition of volatile components in olivines from Yakutian kimberlites of various ages

T2 - Evidence from gas chromatography–mass spectrometry

AU - Tomilenko, A. A.

AU - Bul’bak, T. A.

AU - Khomenko, M. O.

AU - Kuzmin, D. V.

AU - Sobolev, N. V.

PY - 2016/6/1

Y1 - 2016/6/1

N2 - 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.

AB - 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.

UR - http://www.scopus.com/inward/record.url?scp=84978472235&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16060234

DO - 10.1134/S1028334X16060234

M3 - Article

AN - SCOPUS:84978472235

VL - 468

SP - 626

EP - 631

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25763159