Standard

Experimental Modeling of C0-Forming Processes Involving Cohenite and CO2-Fluid in a Silicate Mantle. / Bataleva, Yu V.; Palyanov, Yu N.; Borzdov, Yu M. et al.

In: Doklady Earth Sciences, Vol. 483, No. 1, 01.12.2018, p. 1427-1430.

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

Harvard

Bataleva, YV, Palyanov, YN, Borzdov, YM, Bayukov, OA & Sobolev, NV 2018, 'Experimental Modeling of C0-Forming Processes Involving Cohenite and CO2-Fluid in a Silicate Mantle', Doklady Earth Sciences, vol. 483, no. 1, pp. 1427-1430. https://doi.org/10.1134/S1028334X18110016

APA

Bataleva, Y. V., Palyanov, Y. N., Borzdov, Y. M., Bayukov, O. A., & Sobolev, N. V. (2018). Experimental Modeling of C0-Forming Processes Involving Cohenite and CO2-Fluid in a Silicate Mantle. Doklady Earth Sciences, 483(1), 1427-1430. https://doi.org/10.1134/S1028334X18110016

Vancouver

Bataleva YV, Palyanov YN, Borzdov YM, Bayukov OA, Sobolev NV. Experimental Modeling of C0-Forming Processes Involving Cohenite and CO2-Fluid in a Silicate Mantle. Doklady Earth Sciences. 2018 Dec 1;483(1):1427-1430. doi: 10.1134/S1028334X18110016

Author

Bataleva, Yu V. ; Palyanov, Yu N. ; Borzdov, Yu M. et al. / Experimental Modeling of C0-Forming Processes Involving Cohenite and CO2-Fluid in a Silicate Mantle. In: Doklady Earth Sciences. 2018 ; Vol. 483, No. 1. pp. 1427-1430.

BibTeX

@article{524caa3aff49422f94e70a043cdb0e4a,
title = "Experimental Modeling of C0-Forming Processes Involving Cohenite and CO2-Fluid in a Silicate Mantle",
abstract = "Abstract: Experimental studies were performed in the Fe3C–SiO2–(Mg,Ca)CO3 system (6.3 GPа, 1100–1500°C, 20–40 h). It is established that the carbide–oxide–carbonate interaction leads to the formation of ferrosilite, fayalite, graphite, and cohenite (1100 and 1200°С), as well as a Fe–C melt (1300°С). It is determined that the main processes in the system are decarbonation, redox-reactions of cohenite and a CO2-fluid, extraction of carbon from carbide, and crystallization of metastable graphite (± diamond growth), as well as the formation of ferriferous silicates. The interaction studied can be considered as a simplified model of the processes that occur during the subduction of oxidized crustal material to reduced mantle rocks.",
keywords = "DIAMOND FORMATION, IRON CARBIDE, CARBON, GRAPHITE, MECHANISMS, INCLUSIONS, PARAMETERS, NITROGEN, IMPURITY, GROWTH",
author = "Bataleva, {Yu V.} and Palyanov, {Yu N.} and Borzdov, {Yu M.} and Bayukov, {O. A.} and Sobolev, {N. V.}",
year = "2018",
month = dec,
day = "1",
doi = "10.1134/S1028334X18110016",
language = "English",
volume = "483",
pages = "1427--1430",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Experimental Modeling of C0-Forming Processes Involving Cohenite and CO2-Fluid in a Silicate Mantle

AU - Bataleva, Yu V.

AU - Palyanov, Yu N.

AU - Borzdov, Yu M.

AU - Bayukov, O. A.

AU - Sobolev, N. V.

PY - 2018/12/1

Y1 - 2018/12/1

N2 - Abstract: Experimental studies were performed in the Fe3C–SiO2–(Mg,Ca)CO3 system (6.3 GPа, 1100–1500°C, 20–40 h). It is established that the carbide–oxide–carbonate interaction leads to the formation of ferrosilite, fayalite, graphite, and cohenite (1100 and 1200°С), as well as a Fe–C melt (1300°С). It is determined that the main processes in the system are decarbonation, redox-reactions of cohenite and a CO2-fluid, extraction of carbon from carbide, and crystallization of metastable graphite (± diamond growth), as well as the formation of ferriferous silicates. The interaction studied can be considered as a simplified model of the processes that occur during the subduction of oxidized crustal material to reduced mantle rocks.

AB - Abstract: Experimental studies were performed in the Fe3C–SiO2–(Mg,Ca)CO3 system (6.3 GPа, 1100–1500°C, 20–40 h). It is established that the carbide–oxide–carbonate interaction leads to the formation of ferrosilite, fayalite, graphite, and cohenite (1100 and 1200°С), as well as a Fe–C melt (1300°С). It is determined that the main processes in the system are decarbonation, redox-reactions of cohenite and a CO2-fluid, extraction of carbon from carbide, and crystallization of metastable graphite (± diamond growth), as well as the formation of ferriferous silicates. The interaction studied can be considered as a simplified model of the processes that occur during the subduction of oxidized crustal material to reduced mantle rocks.

KW - DIAMOND FORMATION

KW - IRON CARBIDE

KW - CARBON

KW - GRAPHITE

KW - MECHANISMS

KW - INCLUSIONS

KW - PARAMETERS

KW - NITROGEN

KW - IMPURITY

KW - GROWTH

UR - http://www.scopus.com/inward/record.url?scp=85058858773&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18110016

DO - 10.1134/S1028334X18110016

M3 - Article

AN - SCOPUS:85058858773

VL - 483

SP - 1427

EP - 1430

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 17926998