Inclusions of Cr- and Cr–Nb-Rutile in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia

D. I. Rezvukhin; V. G. Malkovets; I. S. Sharygin; D. V. Kuzmin; K. D. Litasov; A. A. Gibsher; N. P. Pokhilenko; N. V. Sobolev

doi:10.1134/S1028334X1602015X

Inclusions of Cr- and Cr–Nb-Rutile in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia

D. I. Rezvukhin, V. G. Malkovets, I. S. Sharygin, D. V. Kuzmin, K. D. Litasov, A. A. Gibsher, N. P. Pokhilenko, N. V. Sobolev

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

10 Цитирования (Scopus)

Аннотация

The results of study of rutile inclusions in pyrope from the Internatsionalnaya kimberlite pipe are presented. Rutile is characterized by unusually high contents of impurities (up to 25 wt %). The presence of Cr₂O₃ (up to 9.75 wt %) and Nb₂O₅ (up to 15.57 wt %) are most typical. Rutile inclusions often occur in assemblage with Ti-rich oxides: picroilmenite and crichtonite group minerals. The Cr-pyropes with inclusions of rutile, picroilmenite, and crichtonite group minerals were formed in the lithospheric mantle beneath the Mirnyi field during their joint crystallization from melts enriched in Fe, Ti, and other incompatible elements as a result of metasomatic enrichment of the depleted lithospheric mantle.

Язык оригинала	английский
Страницы (с-по)	173-176
Число страниц	4
Журнал	Doklady Earth Sciences
Том	466
Номер выпуска	2
DOI	https://doi.org/10.1134/S1028334X1602015X
Состояние	Опубликовано - 1 февр. 2016

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10.1134/S1028334X1602015X

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title = "Inclusions of Cr- and Cr–Nb-Rutile in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia",

abstract = "The results of study of rutile inclusions in pyrope from the Internatsionalnaya kimberlite pipe are presented. Rutile is characterized by unusually high contents of impurities (up to 25 wt %). The presence of Cr2O3 (up to 9.75 wt %) and Nb2O5 (up to 15.57 wt %) are most typical. Rutile inclusions often occur in assemblage with Ti-rich oxides: picroilmenite and crichtonite group minerals. The Cr-pyropes with inclusions of rutile, picroilmenite, and crichtonite group minerals were formed in the lithospheric mantle beneath the Mirnyi field during their joint crystallization from melts enriched in Fe, Ti, and other incompatible elements as a result of metasomatic enrichment of the depleted lithospheric mantle.",

author = "Rezvukhin, {D. I.} and Malkovets, {V. G.} and Sharygin, {I. S.} and Kuzmin, {D. V.} and Litasov, {K. D.} and Gibsher, {A. A.} and Pokhilenko, {N. P.} and Sobolev, {N. V.}",

year = "2016",

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Inclusions of Cr- and Cr–Nb-Rutile in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia. / Rezvukhin, D. I.; Malkovets, V. G.; Sharygin, I. S. и др.

В: Doklady Earth Sciences, Том 466, № 2, 01.02.2016, стр. 173-176.

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

TY - JOUR

T1 - Inclusions of Cr- and Cr–Nb-Rutile in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia

AU - Rezvukhin, D. I.

AU - Malkovets, V. G.

AU - Sharygin, I. S.

AU - Kuzmin, D. V.

AU - Litasov, K. D.

AU - Gibsher, A. A.

AU - Pokhilenko, N. P.

AU - Sobolev, N. V.

PY - 2016/2/1

Y1 - 2016/2/1

N2 - The results of study of rutile inclusions in pyrope from the Internatsionalnaya kimberlite pipe are presented. Rutile is characterized by unusually high contents of impurities (up to 25 wt %). The presence of Cr2O3 (up to 9.75 wt %) and Nb2O5 (up to 15.57 wt %) are most typical. Rutile inclusions often occur in assemblage with Ti-rich oxides: picroilmenite and crichtonite group minerals. The Cr-pyropes with inclusions of rutile, picroilmenite, and crichtonite group minerals were formed in the lithospheric mantle beneath the Mirnyi field during their joint crystallization from melts enriched in Fe, Ti, and other incompatible elements as a result of metasomatic enrichment of the depleted lithospheric mantle.

AB - The results of study of rutile inclusions in pyrope from the Internatsionalnaya kimberlite pipe are presented. Rutile is characterized by unusually high contents of impurities (up to 25 wt %). The presence of Cr2O3 (up to 9.75 wt %) and Nb2O5 (up to 15.57 wt %) are most typical. Rutile inclusions often occur in assemblage with Ti-rich oxides: picroilmenite and crichtonite group minerals. The Cr-pyropes with inclusions of rutile, picroilmenite, and crichtonite group minerals were formed in the lithospheric mantle beneath the Mirnyi field during their joint crystallization from melts enriched in Fe, Ti, and other incompatible elements as a result of metasomatic enrichment of the depleted lithospheric mantle.

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DO - 10.1134/S1028334X1602015X

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JO - Doklady Earth Sciences

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