Standard

Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia : The problem of the kimberlite melt. / Tomilenko, A. A.; Kuzmin, D. V.; Bul’bak, T. A. et al.

In: Doklady Earth Sciences, Vol. 475, No. 2, 01.08.2017, p. 949-952.

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

Harvard

Tomilenko, AA, Kuzmin, DV, Bul’bak, TA & Sobolev, NV 2017, 'Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia: The problem of the kimberlite melt', Doklady Earth Sciences, vol. 475, no. 2, pp. 949-952. https://doi.org/10.1134/S1028334X17080281

APA

Tomilenko, A. A., Kuzmin, D. V., Bul’bak, T. A., & Sobolev, N. V. (2017). Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia: The problem of the kimberlite melt. Doklady Earth Sciences, 475(2), 949-952. https://doi.org/10.1134/S1028334X17080281

Vancouver

Tomilenko AA, Kuzmin DV, Bul’bak TA, Sobolev NV. Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia: The problem of the kimberlite melt. Doklady Earth Sciences. 2017 Aug 1;475(2):949-952. doi: 10.1134/S1028334X17080281

Author

Tomilenko, A. A. ; Kuzmin, D. V. ; Bul’bak, T. A. et al. / Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia : The problem of the kimberlite melt. In: Doklady Earth Sciences. 2017 ; Vol. 475, No. 2. pp. 949-952.

BibTeX

@article{1d1194b1b5c640dd96012ef304bb506b,
title = "Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia: The problem of the kimberlite melt",
abstract = "The primary melt and fluid inclusions in regenerated zonal crystals of olivine and homogeneous phenocrysts of olivine from kimberlites of the Udachnaya-East pipe, were first studied by means of microthermometry, optic and scanning electron microscopy, electron and ion microprobe analysis (SIMS), inductively coupled plasma mass-spectrometry (ICP MSC), and Raman spectroscopy. It was established that olivine crystals were regenerated from silicate–carbonate melts at a temperature of ~1100°C.",
keywords = "CHROMATOGRAPHY-MASS SPECTROMETRY, HYPABYSSAL KIMBERLITES, VOLATILE COMPONENTS, RUSSIA, AGES",
author = "Tomilenko, {A. A.} and Kuzmin, {D. V.} and Bul{\textquoteright}bak, {T. A.} and Sobolev, {N. V.}",
year = "2017",
month = aug,
day = "1",
doi = "10.1134/S1028334X17080281",
language = "English",
volume = "475",
pages = "949--952",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Primary melt and fluid inclusions in regenerated crystals and phenocrysts of olivine from kimberlites of the Udachnaya-East Pipe, Yakutia

T2 - The problem of the kimberlite melt

AU - Tomilenko, A. A.

AU - Kuzmin, D. V.

AU - Bul’bak, T. A.

AU - Sobolev, N. V.

PY - 2017/8/1

Y1 - 2017/8/1

N2 - The primary melt and fluid inclusions in regenerated zonal crystals of olivine and homogeneous phenocrysts of olivine from kimberlites of the Udachnaya-East pipe, were first studied by means of microthermometry, optic and scanning electron microscopy, electron and ion microprobe analysis (SIMS), inductively coupled plasma mass-spectrometry (ICP MSC), and Raman spectroscopy. It was established that olivine crystals were regenerated from silicate–carbonate melts at a temperature of ~1100°C.

AB - The primary melt and fluid inclusions in regenerated zonal crystals of olivine and homogeneous phenocrysts of olivine from kimberlites of the Udachnaya-East pipe, were first studied by means of microthermometry, optic and scanning electron microscopy, electron and ion microprobe analysis (SIMS), inductively coupled plasma mass-spectrometry (ICP MSC), and Raman spectroscopy. It was established that olivine crystals were regenerated from silicate–carbonate melts at a temperature of ~1100°C.

KW - CHROMATOGRAPHY-MASS SPECTROMETRY

KW - HYPABYSSAL KIMBERLITES

KW - VOLATILE COMPONENTS

KW - RUSSIA

KW - AGES

UR - http://www.scopus.com/inward/record.url?scp=85028747236&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17080281

DO - 10.1134/S1028334X17080281

M3 - Article

AN - SCOPUS:85028747236

VL - 475

SP - 949

EP - 952

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 9915853