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The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts : Experimental modeling under PT-conditions of lithospheric mantle. / Bataleva, Yu V.; Palyanov, Yu N.; Sokol, A. G. et al.

In: Russian Geology and Geophysics, Vol. 56, No. 1-2, 01.01.2015, p. 143-154.

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

Harvard

Bataleva, YV, Palyanov, YN, Sokol, AG, Borzdov, YM & Bayukov, OA 2015, 'The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts: Experimental modeling under PT-conditions of lithospheric mantle', Russian Geology and Geophysics, vol. 56, no. 1-2, pp. 143-154. https://doi.org/10.1016/j.rgg.2015.01.008

APA

Bataleva, Y. V., Palyanov, Y. N., Sokol, A. G., Borzdov, Y. M., & Bayukov, O. A. (2015). The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts: Experimental modeling under PT-conditions of lithospheric mantle. Russian Geology and Geophysics, 56(1-2), 143-154. https://doi.org/10.1016/j.rgg.2015.01.008

Vancouver

Bataleva YV, Palyanov YN, Sokol AG, Borzdov YM, Bayukov OA. The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts: Experimental modeling under PT-conditions of lithospheric mantle. Russian Geology and Geophysics. 2015 Jan 1;56(1-2):143-154. doi: 10.1016/j.rgg.2015.01.008

Author

Bataleva, Yu V. ; Palyanov, Yu N. ; Sokol, A. G. et al. / The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts : Experimental modeling under PT-conditions of lithospheric mantle. In: Russian Geology and Geophysics. 2015 ; Vol. 56, No. 1-2. pp. 143-154.

BibTeX

@article{cdc4da55d5734ffcacc79fa289d950cf,
title = "The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts: Experimental modeling under PT-conditions of lithospheric mantle",
abstract = "Experimental modeling of the processes of formation of ferric carbonate-silicate melts through the carbonate-oxide-metal interaction is performed in the (Mg,Ca)CO3-SiO2-Al2O3-Fe0 system at 6.3 and 7.5GPa and within 1150-1650°C, using a multianvil high-pressure apparatus of {"}split-sphere{"} type (BARS). Two parallel reactions run in the subsolidus region (1150-1450°C): decarbonation, producing pyrope-almandine (Fe#=0.40-0.75) and CO2 fluid, and redox interaction between carbonate and Fe0, resulting in the crystallization of iron carbide in assemblage with magnesiowustite (Fe#=0.75-0.85). It is shown that the reduction of carbonate or CO2 fluid by iron carbide and parallel redox interaction of magnesiowustite with CO2 produce graphite in assemblage with Fe3+-containing magnesiowustite. In the temperature range of 1450-1650°C, generation of carbonate-silicate melts coexisting with pyrope-almandine, magnesiowustite, magnetite, ferrospinel, and graphite takes place. The composition of the produced melts is as follows: SiO2 ≈ 10-15wt.%, X(FeO+Fe2O3)=36-43wt.%, and Fe3+/XFe ≈ 0.18-0.23. These Fe3+-enriched carbonate-silicate melts/fluids are saturated with carbon and are the medium of graphite crystallization. Oxide and silicate phases (almandine, ferrospinel, and magnetite) coexisting with graphite are also characterized by high Fe3+/XFe values. It has been established that Fe3+-enriched carbonate-silicate melts can result from the interaction of Fe0-containing rocks with carbonated rocks. In the reduced mantle (with the presence of iron carbides or oxides), melts of this composition can be the source of carbon and the medium of graphite crystallization at once. After separation and ascent, these ferric carbonate-silicate melts can favor oxidizing metasomatism in the lithospheric mantle.",
keywords = "Carbonate-silicate melt, Garnet, Graphite, High-pressure experiment, Iron carbide, Redox gradient",
author = "Bataleva, {Yu V.} and Palyanov, {Yu N.} and Sokol, {A. G.} and Borzdov, {Yu M.} and Bayukov, {O. A.}",
year = "2015",
month = jan,
day = "1",
doi = "10.1016/j.rgg.2015.01.008",
language = "English",
volume = "56",
pages = "143--154",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "1-2",

}

RIS

TY - JOUR

T1 - The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts

T2 - Experimental modeling under PT-conditions of lithospheric mantle

AU - Bataleva, Yu V.

AU - Palyanov, Yu N.

AU - Sokol, A. G.

AU - Borzdov, Yu M.

AU - Bayukov, O. A.

PY - 2015/1/1

Y1 - 2015/1/1

N2 - Experimental modeling of the processes of formation of ferric carbonate-silicate melts through the carbonate-oxide-metal interaction is performed in the (Mg,Ca)CO3-SiO2-Al2O3-Fe0 system at 6.3 and 7.5GPa and within 1150-1650°C, using a multianvil high-pressure apparatus of "split-sphere" type (BARS). Two parallel reactions run in the subsolidus region (1150-1450°C): decarbonation, producing pyrope-almandine (Fe#=0.40-0.75) and CO2 fluid, and redox interaction between carbonate and Fe0, resulting in the crystallization of iron carbide in assemblage with magnesiowustite (Fe#=0.75-0.85). It is shown that the reduction of carbonate or CO2 fluid by iron carbide and parallel redox interaction of magnesiowustite with CO2 produce graphite in assemblage with Fe3+-containing magnesiowustite. In the temperature range of 1450-1650°C, generation of carbonate-silicate melts coexisting with pyrope-almandine, magnesiowustite, magnetite, ferrospinel, and graphite takes place. The composition of the produced melts is as follows: SiO2 ≈ 10-15wt.%, X(FeO+Fe2O3)=36-43wt.%, and Fe3+/XFe ≈ 0.18-0.23. These Fe3+-enriched carbonate-silicate melts/fluids are saturated with carbon and are the medium of graphite crystallization. Oxide and silicate phases (almandine, ferrospinel, and magnetite) coexisting with graphite are also characterized by high Fe3+/XFe values. It has been established that Fe3+-enriched carbonate-silicate melts can result from the interaction of Fe0-containing rocks with carbonated rocks. In the reduced mantle (with the presence of iron carbides or oxides), melts of this composition can be the source of carbon and the medium of graphite crystallization at once. After separation and ascent, these ferric carbonate-silicate melts can favor oxidizing metasomatism in the lithospheric mantle.

AB - Experimental modeling of the processes of formation of ferric carbonate-silicate melts through the carbonate-oxide-metal interaction is performed in the (Mg,Ca)CO3-SiO2-Al2O3-Fe0 system at 6.3 and 7.5GPa and within 1150-1650°C, using a multianvil high-pressure apparatus of "split-sphere" type (BARS). Two parallel reactions run in the subsolidus region (1150-1450°C): decarbonation, producing pyrope-almandine (Fe#=0.40-0.75) and CO2 fluid, and redox interaction between carbonate and Fe0, resulting in the crystallization of iron carbide in assemblage with magnesiowustite (Fe#=0.75-0.85). It is shown that the reduction of carbonate or CO2 fluid by iron carbide and parallel redox interaction of magnesiowustite with CO2 produce graphite in assemblage with Fe3+-containing magnesiowustite. In the temperature range of 1450-1650°C, generation of carbonate-silicate melts coexisting with pyrope-almandine, magnesiowustite, magnetite, ferrospinel, and graphite takes place. The composition of the produced melts is as follows: SiO2 ≈ 10-15wt.%, X(FeO+Fe2O3)=36-43wt.%, and Fe3+/XFe ≈ 0.18-0.23. These Fe3+-enriched carbonate-silicate melts/fluids are saturated with carbon and are the medium of graphite crystallization. Oxide and silicate phases (almandine, ferrospinel, and magnetite) coexisting with graphite are also characterized by high Fe3+/XFe values. It has been established that Fe3+-enriched carbonate-silicate melts can result from the interaction of Fe0-containing rocks with carbonated rocks. In the reduced mantle (with the presence of iron carbides or oxides), melts of this composition can be the source of carbon and the medium of graphite crystallization at once. After separation and ascent, these ferric carbonate-silicate melts can favor oxidizing metasomatism in the lithospheric mantle.

KW - Carbonate-silicate melt

KW - Garnet

KW - Graphite

KW - High-pressure experiment

KW - Iron carbide

KW - Redox gradient

UR - http://www.scopus.com/inward/record.url?scp=84925300371&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2015.01.008

DO - 10.1016/j.rgg.2015.01.008

M3 - Article

AN - SCOPUS:84925300371

VL - 56

SP - 143

EP - 154

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 1-2

ER -

ID: 25728075