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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. et al.

In: Doklady Earth Sciences, Vol. 466, No. 2, 01.02.2016, p. 173-176.

Research output: Contribution to journal › Article › peer-review

Harvard

Rezvukhin, DI, Malkovets, VG, Sharygin, IS, Kuzmin, DV, Litasov, KD, Gibsher, AA, Pokhilenko, NP & Sobolev, NV 2016, 'Inclusions of Cr- and Cr–Nb-Rutile in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia', Doklady Earth Sciences, vol. 466, no. 2, pp. 173-176. https://doi.org/10.1134/S1028334X1602015X

APA

Rezvukhin, D. I., Malkovets, V. G., Sharygin, I. S., Kuzmin, D. V., Litasov, K. D., Gibsher, A. A., Pokhilenko, N. P., & Sobolev, N. V. (2016). Inclusions of Cr- and Cr–Nb-Rutile in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia. Doklady Earth Sciences, 466(2), 173-176. https://doi.org/10.1134/S1028334X1602015X

Vancouver

Rezvukhin DI, Malkovets VG, Sharygin IS, Kuzmin DV, Litasov KD, Gibsher AA et al. Inclusions of Cr- and Cr–Nb-Rutile in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia. Doklady Earth Sciences. 2016 Feb 1;466(2):173-176. doi: 10.1134/S1028334X1602015X

Author

Rezvukhin, D. I. ; Malkovets, V. G. ; Sharygin, I. S. et al. / Inclusions of Cr- and Cr–Nb-Rutile in pyropes from the Internatsionalnaya kimberlite pipe, Yakutia. In: Doklady Earth Sciences. 2016 ; Vol. 466, No. 2. pp. 173-176.

BibTeX

@article{d9c92e74800043bc9262d1e3e2635e3c,
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",
month = feb,
day = "1",
doi = "10.1134/S1028334X1602015X",
language = "English",
volume = "466",
pages = "173--176",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

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.

UR - http://www.scopus.com/inward/record.url?scp=84962637622&partnerID=8YFLogxK

U2 - 10.1134/S1028334X1602015X

DO - 10.1134/S1028334X1602015X

M3 - Article

AN - SCOPUS:84962637622

VL - 466

SP - 173

EP - 176

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25756393