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Experimental modeling of the interaction of subducted carbonates and sulfur with mantle silicates. / Bataleva, Yu V.; Palyanov, Yu N.; Borzdov, Yu M. et al.

In: Doklady Earth Sciences, Vol. 470, No. 1, 01.09.2016, p. 953-956.

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

Harvard

Bataleva, YV, Palyanov, YN, Borzdov, YM, Zdrokov, EV & Sobolev, NV 2016, 'Experimental modeling of the interaction of subducted carbonates and sulfur with mantle silicates', Doklady Earth Sciences, vol. 470, no. 1, pp. 953-956. https://doi.org/10.1134/S1028334X16090105

APA

Bataleva, Y. V., Palyanov, Y. N., Borzdov, Y. M., Zdrokov, E. V., & Sobolev, N. V. (2016). Experimental modeling of the interaction of subducted carbonates and sulfur with mantle silicates. Doklady Earth Sciences, 470(1), 953-956. https://doi.org/10.1134/S1028334X16090105

Vancouver

Bataleva YV, Palyanov YN, Borzdov YM, Zdrokov EV, Sobolev NV. Experimental modeling of the interaction of subducted carbonates and sulfur with mantle silicates. Doklady Earth Sciences. 2016 Sept 1;470(1):953-956. doi: 10.1134/S1028334X16090105

Author

Bataleva, Yu V. ; Palyanov, Yu N. ; Borzdov, Yu M. et al. / Experimental modeling of the interaction of subducted carbonates and sulfur with mantle silicates. In: Doklady Earth Sciences. 2016 ; Vol. 470, No. 1. pp. 953-956.

BibTeX

@article{04186dcf8c3c46b1b8db374637ad9cc4,
title = "Experimental modeling of the interaction of subducted carbonates and sulfur with mantle silicates",
abstract = "Experimental studies in the system Fe,Ni–olivine–carbonate–S (P = 6.3 GPa, T = 1050–1550°C, t = 40–60 h) aimed at modeling of the interaction of subducted carbonates and sulfur with rocks of the silicate mantle and at investigation of the likely mechanism of the formation of mantle sulfides were performed. It is shown that an association of olivine + orthopyroxene + magnesite + pyrite coexisting with a sulfur melt/fluid with dissolved Fe, Ni, and O is formed at T ≤ 1250°C. An association of low-Fe olivine, orthopyroxene, and magnesite and two immiscible melts of the carbonate and S–Fe–Ni–O compositions are formed at T ≥ 1350°C. It is shown that the reduced S-bearing fluids may transform silicates and carbonates, extract metals from the solid-phase matrix, and provide conditions for generation of sulfide melts.",
author = "Bataleva, {Yu V.} and Palyanov, {Yu N.} and Borzdov, {Yu M.} and Zdrokov, {E. V.} and Sobolev, {N. V.}",
year = "2016",
month = sep,
day = "1",
doi = "10.1134/S1028334X16090105",
language = "English",
volume = "470",
pages = "953--956",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Experimental modeling of the interaction of subducted carbonates and sulfur with mantle silicates

AU - Bataleva, Yu V.

AU - Palyanov, Yu N.

AU - Borzdov, Yu M.

AU - Zdrokov, E. V.

AU - Sobolev, N. V.

PY - 2016/9/1

Y1 - 2016/9/1

N2 - Experimental studies in the system Fe,Ni–olivine–carbonate–S (P = 6.3 GPa, T = 1050–1550°C, t = 40–60 h) aimed at modeling of the interaction of subducted carbonates and sulfur with rocks of the silicate mantle and at investigation of the likely mechanism of the formation of mantle sulfides were performed. It is shown that an association of olivine + orthopyroxene + magnesite + pyrite coexisting with a sulfur melt/fluid with dissolved Fe, Ni, and O is formed at T ≤ 1250°C. An association of low-Fe olivine, orthopyroxene, and magnesite and two immiscible melts of the carbonate and S–Fe–Ni–O compositions are formed at T ≥ 1350°C. It is shown that the reduced S-bearing fluids may transform silicates and carbonates, extract metals from the solid-phase matrix, and provide conditions for generation of sulfide melts.

AB - Experimental studies in the system Fe,Ni–olivine–carbonate–S (P = 6.3 GPa, T = 1050–1550°C, t = 40–60 h) aimed at modeling of the interaction of subducted carbonates and sulfur with rocks of the silicate mantle and at investigation of the likely mechanism of the formation of mantle sulfides were performed. It is shown that an association of olivine + orthopyroxene + magnesite + pyrite coexisting with a sulfur melt/fluid with dissolved Fe, Ni, and O is formed at T ≤ 1250°C. An association of low-Fe olivine, orthopyroxene, and magnesite and two immiscible melts of the carbonate and S–Fe–Ni–O compositions are formed at T ≥ 1350°C. It is shown that the reduced S-bearing fluids may transform silicates and carbonates, extract metals from the solid-phase matrix, and provide conditions for generation of sulfide melts.

UR - http://www.scopus.com/inward/record.url?scp=84991264802&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16090105

DO - 10.1134/S1028334X16090105

M3 - Article

AN - SCOPUS:84991264802

VL - 470

SP - 953

EP - 956

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 25723985