Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Peculiarities of the composition of volatile components in picroilmenites from Yakutian kimberlites of various ages (by gas chromatography—mass spectrometry). / Tomilenko, A. A.; Bul’bak, T. A.; Pokhilenko, L. N. и др.
в: Doklady Earth Sciences, Том 469, № 1, 01.07.2016, стр. 690-694.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Peculiarities of the composition of volatile components in picroilmenites from Yakutian kimberlites of various ages (by gas chromatography—mass spectrometry)
AU - Tomilenko, A. A.
AU - Bul’bak, T. A.
AU - Pokhilenko, L. N.
AU - Kuzmin, D. V.
AU - Sobolev, N. V.
PY - 2016/7/1
Y1 - 2016/7/1
N2 - The composition of volatile components in picroilmenites from Yakutian kimberlitic pipes of various ages (the Olivinovaya, Malokuonapskaya, and Udachnaya–East pipes) was studied for the first time by means of gas chromatography–mass spectrometry (GC-MS). It was shown that picroilmenites and olivines from same kimberlitic pipes contained volatile components of close composition, whereas these components were quite different in these minerals from different pipes. These features point to a common source and represent the specificity of the magma chamber formed under the pronounced influence of hydrocarbons with their derivates, as well as nitrogen-, chlorine-, and sulfur-containing compounds. The fraction of hydrocarbons and derivates in the composition of volatile matter is as high as 99%, including 9.7% of chlorine- and fluorinecontaining compounds.
AB - The composition of volatile components in picroilmenites from Yakutian kimberlitic pipes of various ages (the Olivinovaya, Malokuonapskaya, and Udachnaya–East pipes) was studied for the first time by means of gas chromatography–mass spectrometry (GC-MS). It was shown that picroilmenites and olivines from same kimberlitic pipes contained volatile components of close composition, whereas these components were quite different in these minerals from different pipes. These features point to a common source and represent the specificity of the magma chamber formed under the pronounced influence of hydrocarbons with their derivates, as well as nitrogen-, chlorine-, and sulfur-containing compounds. The fraction of hydrocarbons and derivates in the composition of volatile matter is as high as 99%, including 9.7% of chlorine- and fluorinecontaining compounds.
UR - http://www.scopus.com/inward/record.url?scp=84980413850&partnerID=8YFLogxK
U2 - 10.1134/S1028334X16070084
DO - 10.1134/S1028334X16070084
M3 - Article
AN - SCOPUS:84980413850
VL - 469
SP - 690
EP - 694
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 1
ER -
ID: 25763067