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

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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. и др.

в: Doklady Earth Sciences, Том 463, № 1, 04.07.2015, стр. 677-679.

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

Author

Zhimulev, E. I. ; Chepurov, A. I. ; Sonin, V. M. и др. / Migration of molten iron through an olivine matrix in the presence of carbon at high P–T parameters (experimental data). в: Doklady Earth Sciences. 2015 ; Том 463, № 1. стр. 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