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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.

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

Harvard

Rezvukhin, DI, Malkovets, VG, Sharygin, IS, Kuzmin, DV, Gibsher, AA, Litasov, KD, Pokhilenko, NP & Sobolev, NV 2016, 'Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia', Doklady Earth Sciences, Том. 466, № 2, стр. 206-209. https://doi.org/10.1134/S1028334X16020227

APA

Rezvukhin, D. I., Malkovets, V. G., Sharygin, I. S., Kuzmin, D. V., Gibsher, A. A., Litasov, K. D., Pokhilenko, N. P., & Sobolev, N. V. (2016). Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia. Doklady Earth Sciences, 466(2), 206-209. https://doi.org/10.1134/S1028334X16020227

Vancouver

Rezvukhin DI, Malkovets VG, Sharygin IS, Kuzmin DV, Gibsher AA, Litasov KD и др. Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia. Doklady Earth Sciences. 2016 февр. 1;466(2):206-209. doi: 10.1134/S1028334X16020227

Author

Rezvukhin, D. I. ; Malkovets, V. G. ; Sharygin, I. S. и др. / Inclusions of crichtonite group minerals in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia. в: Doklady Earth Sciences. 2016 ; Том 466, № 2. стр. 206-209.

BibTeX

@article{6cd9902ea5b04def9da5fbd522a0fd94,
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",
month = feb,
day = "1",
doi = "10.1134/S1028334X16020227",
language = "English",
volume = "466",
pages = "206--209",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

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.

UR - http://www.scopus.com/inward/record.url?scp=84962762010&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16020227

DO - 10.1134/S1028334X16020227

M3 - Article

AN - SCOPUS:84962762010

VL - 466

SP - 206

EP - 209

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25756185