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 -