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Composition of primary fluid and melt inclusions in regenerated olivines from hypabyssal kimberlites of the Malokuonapskaya pipe (Yakutia). / Tomilenko, A. A.; Kuzmin, D. V.; Bulbak, T. A. et al.

In: Doklady Earth Sciences, Vol. 465, No. 1, 01.11.2015, p. 1168-1171.

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

Harvard

Tomilenko, AA, Kuzmin, DV, Bulbak, TA, Timina, TY & Sobolev, NV 2015, 'Composition of primary fluid and melt inclusions in regenerated olivines from hypabyssal kimberlites of the Malokuonapskaya pipe (Yakutia)', Doklady Earth Sciences, vol. 465, no. 1, pp. 1168-1171. https://doi.org/10.1134/S1028334X1511015X

APA

Tomilenko, A. A., Kuzmin, D. V., Bulbak, T. A., Timina, T. Y., & Sobolev, N. V. (2015). Composition of primary fluid and melt inclusions in regenerated olivines from hypabyssal kimberlites of the Malokuonapskaya pipe (Yakutia). Doklady Earth Sciences, 465(1), 1168-1171. https://doi.org/10.1134/S1028334X1511015X

Vancouver

Tomilenko AA, Kuzmin DV, Bulbak TA, Timina TY, Sobolev NV. Composition of primary fluid and melt inclusions in regenerated olivines from hypabyssal kimberlites of the Malokuonapskaya pipe (Yakutia). Doklady Earth Sciences. 2015 Nov 1;465(1):1168-1171. doi: 10.1134/S1028334X1511015X

Author

Tomilenko, A. A. ; Kuzmin, D. V. ; Bulbak, T. A. et al. / Composition of primary fluid and melt inclusions in regenerated olivines from hypabyssal kimberlites of the Malokuonapskaya pipe (Yakutia). In: Doklady Earth Sciences. 2015 ; Vol. 465, No. 1. pp. 1168-1171.

BibTeX

@article{f566eeb595b04791bd722301c60da0f0,
title = "Composition of primary fluid and melt inclusions in regenerated olivines from hypabyssal kimberlites of the Malokuonapskaya pipe (Yakutia)",
abstract = "The primary fluid and melt inclusions in regenerated zonal crystals of olivine from kimberlites of the Malokuonapskaya pipe were first examined by means of microthermometry, optic and scanning electron microscopy, and Raman spectroscopy. The high-pressure genesis of homogenous central parts of the olivines was revealed, probably under intense metasomatism at early hypogene stages with subsequent regeneration in the kimberlitic melt. The olivine crystals were regenerated from silicate–carbonate melts at about 1100°C. The composition of the kimberlitic melt was changed by way of an increase in the calcium content.",
author = "Tomilenko, {A. A.} and Kuzmin, {D. V.} and Bulbak, {T. A.} and Timina, {T. Yu} and Sobolev, {N. V.}",
year = "2015",
month = nov,
day = "1",
doi = "10.1134/S1028334X1511015X",
language = "English",
volume = "465",
pages = "1168--1171",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Composition of primary fluid and melt inclusions in regenerated olivines from hypabyssal kimberlites of the Malokuonapskaya pipe (Yakutia)

AU - Tomilenko, A. A.

AU - Kuzmin, D. V.

AU - Bulbak, T. A.

AU - Timina, T. Yu

AU - Sobolev, N. V.

PY - 2015/11/1

Y1 - 2015/11/1

N2 - The primary fluid and melt inclusions in regenerated zonal crystals of olivine from kimberlites of the Malokuonapskaya pipe were first examined by means of microthermometry, optic and scanning electron microscopy, and Raman spectroscopy. The high-pressure genesis of homogenous central parts of the olivines was revealed, probably under intense metasomatism at early hypogene stages with subsequent regeneration in the kimberlitic melt. The olivine crystals were regenerated from silicate–carbonate melts at about 1100°C. The composition of the kimberlitic melt was changed by way of an increase in the calcium content.

AB - The primary fluid and melt inclusions in regenerated zonal crystals of olivine from kimberlites of the Malokuonapskaya pipe were first examined by means of microthermometry, optic and scanning electron microscopy, and Raman spectroscopy. The high-pressure genesis of homogenous central parts of the olivines was revealed, probably under intense metasomatism at early hypogene stages with subsequent regeneration in the kimberlitic melt. The olivine crystals were regenerated from silicate–carbonate melts at about 1100°C. The composition of the kimberlitic melt was changed by way of an increase in the calcium content.

UR - http://www.scopus.com/inward/record.url?scp=84951061922&partnerID=8YFLogxK

U2 - 10.1134/S1028334X1511015X

DO - 10.1134/S1028334X1511015X

M3 - Article

AN - SCOPUS:84951061922

VL - 465

SP - 1168

EP - 1171

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 25763507