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Migration of molten iron through an olivine matrix in the presence of carbon at high P–T parameters (experimental data). / Zhimulev, E. I.; Chepurov, A. I.; Sonin, V. M. et al.

In: Doklady Earth Sciences, Vol. 463, No. 1, 04.07.2015, p. 677-679.

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

Harvard

Zhimulev, EI, Chepurov, AI, Sonin, VM & Pokhilenko, NP 2015, 'Migration of molten iron through an olivine matrix in the presence of carbon at high P–T parameters (experimental data)', Doklady Earth Sciences, vol. 463, no. 1, pp. 677-679. https://doi.org/10.1134/S1028334X15070065

APA

Zhimulev, E. I., Chepurov, A. I., Sonin, V. M., & Pokhilenko, N. P. (2015). Migration of molten iron through an olivine matrix in the presence of carbon at high P–T parameters (experimental data). Doklady Earth Sciences, 463(1), 677-679. https://doi.org/10.1134/S1028334X15070065

Vancouver

Zhimulev EI, Chepurov AI, Sonin VM, Pokhilenko NP. Migration of molten iron through an olivine matrix in the presence of carbon at high P–T parameters (experimental data). Doklady Earth Sciences. 2015 Jul 4;463(1):677-679. doi: 10.1134/S1028334X15070065

Author

Zhimulev, E. I. ; Chepurov, A. I. ; Sonin, V. M. et al. / Migration of molten iron through an olivine matrix in the presence of carbon at high P–T parameters (experimental data). In: Doklady Earth Sciences. 2015 ; Vol. 463, No. 1. pp. 677-679.

BibTeX

@article{d928ab5662314251b0634c0faa9000e8,
title = "Migration of molten iron through an olivine matrix in the presence of carbon at high P–T parameters (experimental data)",
abstract = "This report presents the primary results of experiments at 5.5 GPa and 1600°C on the migration of molten iron through a solid silicate matrix consisting of olivine crystals with graphite-filled interstices. It was shown that the migration rate was quite high at the given P and T values (up to 2.5 mm/h). It was shown that carbon in its elemental forms might affect the migration capability of molten iron. This effect must be included in creating a correct model of the formation of the inner parts of the Earth, the terrestrial planets, and planetoids.",
author = "Zhimulev, {E. I.} and Chepurov, {A. I.} and Sonin, {V. M.} and Pokhilenko, {N. P.}",
year = "2015",
month = jul,
day = "4",
doi = "10.1134/S1028334X15070065",
language = "English",
volume = "463",
pages = "677--679",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Migration of molten iron through an olivine matrix in the presence of carbon at high P–T parameters (experimental data)

AU - Zhimulev, E. I.

AU - Chepurov, A. I.

AU - Sonin, V. M.

AU - Pokhilenko, N. P.

PY - 2015/7/4

Y1 - 2015/7/4

N2 - This report presents the primary results of experiments at 5.5 GPa and 1600°C on the migration of molten iron through a solid silicate matrix consisting of olivine crystals with graphite-filled interstices. It was shown that the migration rate was quite high at the given P and T values (up to 2.5 mm/h). It was shown that carbon in its elemental forms might affect the migration capability of molten iron. This effect must be included in creating a correct model of the formation of the inner parts of the Earth, the terrestrial planets, and planetoids.

AB - This report presents the primary results of experiments at 5.5 GPa and 1600°C on the migration of molten iron through a solid silicate matrix consisting of olivine crystals with graphite-filled interstices. It was shown that the migration rate was quite high at the given P and T values (up to 2.5 mm/h). It was shown that carbon in its elemental forms might affect the migration capability of molten iron. This effect must be included in creating a correct model of the formation of the inner parts of the Earth, the terrestrial planets, and planetoids.

UR - http://www.scopus.com/inward/record.url?scp=84938490549&partnerID=8YFLogxK

U2 - 10.1134/S1028334X15070065

DO - 10.1134/S1028334X15070065

M3 - Article

AN - SCOPUS:84938490549

VL - 463

SP - 677

EP - 679

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 25756931