Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia

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

doi:10.1134/S1028334X16020227

Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia

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

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

4 Цитирования (Scopus)

Аннотация

The results of study of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe are reported. Most of the studied samples are characterized by high concentrations of Sr, Ca, Na, and LREEs in comparison with minerals of the LIMA series from kimberlites of South Africa, whereas the average concentrations of Ba and K are significantly lower. Crichtonite group minerals in pyropes are characterized by predomination of Na over K in most samples and by a high concentration of Al₂O₃ (up to 4.5 wt %). Findings of inclusions of crichtonite group minerals with high concentrations of incompatible elements provide evidence for the metasomatic origin of host chromium-rich pyropes.

Язык оригинала	английский
Страницы (с-по)	206-209
Число страниц	4
Журнал	Doklady Earth Sciences
Том	466
Номер выпуска	2
DOI	https://doi.org/10.1134/S1028334X16020227
Состояние	Опубликовано - 1 февр. 2016

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10.1134/S1028334X16020227

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title = "Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia",

abstract = "The results of study of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe are reported. Most of the studied samples are characterized by high concentrations of Sr, Ca, Na, and LREEs in comparison with minerals of the LIMA series from kimberlites of South Africa, whereas the average concentrations of Ba and K are significantly lower. Crichtonite group minerals in pyropes are characterized by predomination of Na over K in most samples and by a high concentration of Al2O3 (up to 4.5 wt %). Findings of inclusions of crichtonite group minerals with high concentrations of incompatible elements provide evidence for the metasomatic origin of host chromium-rich pyropes.",

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

year = "2016",

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doi = "10.1134/S1028334X16020227",

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Inclusions of crichtonite group minerals 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. 206-209.

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

TY - JOUR

T1 - Inclusions of crichtonite group minerals 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 - Gibsher, A. A.

AU - Litasov, K. D.

AU - Pokhilenko, N. P.

AU - Sobolev, N. V.

PY - 2016/2/1

Y1 - 2016/2/1

N2 - The results of study of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe are reported. Most of the studied samples are characterized by high concentrations of Sr, Ca, Na, and LREEs in comparison with minerals of the LIMA series from kimberlites of South Africa, whereas the average concentrations of Ba and K are significantly lower. Crichtonite group minerals in pyropes are characterized by predomination of Na over K in most samples and by a high concentration of Al2O3 (up to 4.5 wt %). Findings of inclusions of crichtonite group minerals with high concentrations of incompatible elements provide evidence for the metasomatic origin of host chromium-rich pyropes.

AB - The results of study of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe are reported. Most of the studied samples are characterized by high concentrations of Sr, Ca, Na, and LREEs in comparison with minerals of the LIMA series from kimberlites of South Africa, whereas the average concentrations of Ba and K are significantly lower. Crichtonite group minerals in pyropes are characterized by predomination of Na over K in most samples and by a high concentration of Al2O3 (up to 4.5 wt %). Findings of inclusions of crichtonite group minerals with high concentrations of incompatible elements provide evidence for the metasomatic origin of host chromium-rich pyropes.

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