High-pressure Raman study of nyerereite from Oldoinyo Lengai

Standard

High-pressure Raman study of nyerereite from Oldoinyo Lengai. / Rashchenko, Sergey V.; Goryainov, Sergey V.; Romanenko, Alexander V. et al.

In: Journal of Raman Spectroscopy, Vol. 48, No. 11, 01.11.2017, p. 1438-1442.

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

Harvard

Rashchenko, SV, Goryainov, SV, Romanenko, AV, Golovin, AV, Korsakov, AV, Moine, BN & Mikhno, AO 2017, 'High-pressure Raman study of nyerereite from Oldoinyo Lengai', Journal of Raman Spectroscopy, vol. 48, no. 11, pp. 1438-1442. https://doi.org/10.1002/jrs.5152

APA

Rashchenko, S. V., Goryainov, S. V., Romanenko, A. V., Golovin, A. V., Korsakov, A. V., Moine, B. N., & Mikhno, A. O. (2017). High-pressure Raman study of nyerereite from Oldoinyo Lengai. Journal of Raman Spectroscopy, 48(11), 1438-1442. https://doi.org/10.1002/jrs.5152

Vancouver

Rashchenko SV, Goryainov SV, Romanenko AV, Golovin AV, Korsakov AV, Moine BN et al. High-pressure Raman study of nyerereite from Oldoinyo Lengai. Journal of Raman Spectroscopy. 2017 Nov 1;48(11):1438-1442. doi: 10.1002/jrs.5152

Author

Rashchenko, Sergey V. ; Goryainov, Sergey V. ; Romanenko, Alexander V. et al. / High-pressure Raman study of nyerereite from Oldoinyo Lengai. In: Journal of Raman Spectroscopy. 2017 ; Vol. 48, No. 11. pp. 1438-1442.

BibTeX

@article{275b7cd02218480f8e6ec7d04fe04839,

title = "High-pressure Raman study of nyerereite from Oldoinyo Lengai",

abstract = "A rare sodium carbonate nyerereite, (Na,K)2Ca(CO3)2, first found in unique natrocarbonatite lava of Oldoinyo Lengai volcano, also attracted a lot of attention as an inclusion phase in mantle minerals formed in the course of deep carbonatite magmatism. We measured the evolution of nyerereite Raman spectra under quasi-hydrostatic compression up to 6.4 GPa using a diamond anvil cell. The ν4(CO3 2−) band (710 cm−1 at ambient pressure) and ν1(CO3 2−) doublet (1077 and 1086 cm−1 at ambient pressure) demonstrated a positive pressure shift with dν/dP irregularities at 0.5 and 3.0 GPa. The obtained calibration was then used for residual pressure measurements in nyerereite-bearing inclusions in olivine from the Udachnaya-East kimberlite.",

keywords = "carbonate, diamond anvil cell, high pressure, nyerereite, Raman spectroscopy, INCLUSIONS, MANTLE MINERALS, VOLCANO, TANZANIA",

author = "Rashchenko, {Sergey V.} and Goryainov, {Sergey V.} and Romanenko, {Alexander V.} and Golovin, {Alexander V.} and Korsakov, {Andrey V.} and Moine, {Bertrand N.} and Mikhno, {Anastasia O.}",

note = "Publisher Copyright: Copyright {\textcopyright} 2017 John Wiley & Sons, Ltd.",

year = "2017",

month = nov,

day = "1",

doi = "10.1002/jrs.5152",

language = "English",

volume = "48",

pages = "1438--1442",

journal = "Journal of Raman Spectroscopy",

issn = "0377-0486",

publisher = "John Wiley and Sons Ltd",

number = "11",

}

RIS

TY - JOUR

T1 - High-pressure Raman study of nyerereite from Oldoinyo Lengai

AU - Rashchenko, Sergey V.

AU - Goryainov, Sergey V.

AU - Romanenko, Alexander V.

AU - Golovin, Alexander V.

AU - Korsakov, Andrey V.

AU - Moine, Bertrand N.

AU - Mikhno, Anastasia O.

PY - 2017/11/1

Y1 - 2017/11/1

N2 - A rare sodium carbonate nyerereite, (Na,K)2Ca(CO3)2, first found in unique natrocarbonatite lava of Oldoinyo Lengai volcano, also attracted a lot of attention as an inclusion phase in mantle minerals formed in the course of deep carbonatite magmatism. We measured the evolution of nyerereite Raman spectra under quasi-hydrostatic compression up to 6.4 GPa using a diamond anvil cell. The ν4(CO3 2−) band (710 cm−1 at ambient pressure) and ν1(CO3 2−) doublet (1077 and 1086 cm−1 at ambient pressure) demonstrated a positive pressure shift with dν/dP irregularities at 0.5 and 3.0 GPa. The obtained calibration was then used for residual pressure measurements in nyerereite-bearing inclusions in olivine from the Udachnaya-East kimberlite.

AB - A rare sodium carbonate nyerereite, (Na,K)2Ca(CO3)2, first found in unique natrocarbonatite lava of Oldoinyo Lengai volcano, also attracted a lot of attention as an inclusion phase in mantle minerals formed in the course of deep carbonatite magmatism. We measured the evolution of nyerereite Raman spectra under quasi-hydrostatic compression up to 6.4 GPa using a diamond anvil cell. The ν4(CO3 2−) band (710 cm−1 at ambient pressure) and ν1(CO3 2−) doublet (1077 and 1086 cm−1 at ambient pressure) demonstrated a positive pressure shift with dν/dP irregularities at 0.5 and 3.0 GPa. The obtained calibration was then used for residual pressure measurements in nyerereite-bearing inclusions in olivine from the Udachnaya-East kimberlite.

KW - carbonate

KW - diamond anvil cell

KW - high pressure

KW - nyerereite

KW - Raman spectroscopy

KW - INCLUSIONS

KW - MANTLE MINERALS

KW - VOLCANO

KW - TANZANIA

UR - http://www.scopus.com/inward/record.url?scp=85017544231&partnerID=8YFLogxK

U2 - 10.1002/jrs.5152

DO - 10.1002/jrs.5152

M3 - Article

AN - SCOPUS:85017544231

VL - 48

SP - 1438

EP - 1442

JO - Journal of Raman Spectroscopy

JF - Journal of Raman Spectroscopy

SN - 0377-0486

IS - 11

ER -

ID: 9953002