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Conditions of carbonation and wehrlitization of lithospheric peridotite upon interaction with carbonatitic melts. / Sokol, A. G.; Kruk, A. N.; Chebotarev, D. A. и др.

в: Doklady Earth Sciences, Том 465, № 2, 01.12.2015, стр. 1262-1267.

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

Harvard

Sokol, AG, Kruk, AN, Chebotarev, DA, Palyanov, YN & Sobolev, NV 2015, 'Conditions of carbonation and wehrlitization of lithospheric peridotite upon interaction with carbonatitic melts', Doklady Earth Sciences, Том. 465, № 2, стр. 1262-1267. https://doi.org/10.1134/S1028334X15120144

APA

Sokol, A. G., Kruk, A. N., Chebotarev, D. A., Palyanov, Y. N., & Sobolev, N. V. (2015). Conditions of carbonation and wehrlitization of lithospheric peridotite upon interaction with carbonatitic melts. Doklady Earth Sciences, 465(2), 1262-1267. https://doi.org/10.1134/S1028334X15120144

Vancouver

Sokol AG, Kruk AN, Chebotarev DA, Palyanov YN, Sobolev NV. Conditions of carbonation and wehrlitization of lithospheric peridotite upon interaction with carbonatitic melts. Doklady Earth Sciences. 2015 дек. 1;465(2):1262-1267. doi: 10.1134/S1028334X15120144

Author

Sokol, A. G. ; Kruk, A. N. ; Chebotarev, D. A. и др. / Conditions of carbonation and wehrlitization of lithospheric peridotite upon interaction with carbonatitic melts. в: Doklady Earth Sciences. 2015 ; Том 465, № 2. стр. 1262-1267.

BibTeX

@article{1ada882668a749ecb0819c6eda675bfe,
title = "Conditions of carbonation and wehrlitization of lithospheric peridotite upon interaction with carbonatitic melts",
abstract = "Study of the mechanism of carbonation and wehrlitization of harzburgite upon metasomatism by carbonatitic melts of various genesis was carried out. Experiments with durations of 60–150 h were performed at 6.3 GPa and 1200°C. The data showed that carbonatite with MgO/CaO > 0.3 percolating into the peridotitic lithosphere may provide crystallization of magnesite in it. The influence of all studied carbonatites results in wehrlitization of peridotite. The compositions of melts formed by interaction with harzburgite (∼2 wt % SiO2, Ca# = 36–47) practically do not depend on the composition of the initial carbonatite. Based on the data obtained, we conclude that the formation of magnesite-bearing and magnesite-free metasomatized peridotites may have a significant influence on the CO2 regime in the further generation of kimberlitic magmas of groups I and II.",
author = "Sokol, {A. G.} and Kruk, {A. N.} and Chebotarev, {D. A.} and Palyanov, {Yu N.} and Sobolev, {N. V.}",
year = "2015",
month = dec,
day = "1",
doi = "10.1134/S1028334X15120144",
language = "English",
volume = "465",
pages = "1262--1267",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Conditions of carbonation and wehrlitization of lithospheric peridotite upon interaction with carbonatitic melts

AU - Sokol, A. G.

AU - Kruk, A. N.

AU - Chebotarev, D. A.

AU - Palyanov, Yu N.

AU - Sobolev, N. V.

PY - 2015/12/1

Y1 - 2015/12/1

N2 - Study of the mechanism of carbonation and wehrlitization of harzburgite upon metasomatism by carbonatitic melts of various genesis was carried out. Experiments with durations of 60–150 h were performed at 6.3 GPa and 1200°C. The data showed that carbonatite with MgO/CaO > 0.3 percolating into the peridotitic lithosphere may provide crystallization of magnesite in it. The influence of all studied carbonatites results in wehrlitization of peridotite. The compositions of melts formed by interaction with harzburgite (∼2 wt % SiO2, Ca# = 36–47) practically do not depend on the composition of the initial carbonatite. Based on the data obtained, we conclude that the formation of magnesite-bearing and magnesite-free metasomatized peridotites may have a significant influence on the CO2 regime in the further generation of kimberlitic magmas of groups I and II.

AB - Study of the mechanism of carbonation and wehrlitization of harzburgite upon metasomatism by carbonatitic melts of various genesis was carried out. Experiments with durations of 60–150 h were performed at 6.3 GPa and 1200°C. The data showed that carbonatite with MgO/CaO > 0.3 percolating into the peridotitic lithosphere may provide crystallization of magnesite in it. The influence of all studied carbonatites results in wehrlitization of peridotite. The compositions of melts formed by interaction with harzburgite (∼2 wt % SiO2, Ca# = 36–47) practically do not depend on the composition of the initial carbonatite. Based on the data obtained, we conclude that the formation of magnesite-bearing and magnesite-free metasomatized peridotites may have a significant influence on the CO2 regime in the further generation of kimberlitic magmas of groups I and II.

UR - http://www.scopus.com/inward/record.url?scp=84953209163&partnerID=8YFLogxK

U2 - 10.1134/S1028334X15120144

DO - 10.1134/S1028334X15120144

M3 - Article

AN - SCOPUS:84953209163

VL - 465

SP - 1262

EP - 1267

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25725878