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


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2018-12

AUTHORS

Yu. V. Bataleva, Yu. N. Palyanov, Yu. M. Borzdov, O. A. Bayukov, N. V. Sobolev

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. More... »

PAGES

1427-1430

Journal

TITLE

Doklady Earth Sciences

ISSUE

1

VOLUME

483

From Grant

  • Identifiers

    URI

    http://scigraph.springernature.com/pub.10.1134/s1028334x18110016

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    http://dx.doi.org/10.1134/s1028334x18110016

    DIMENSIONS

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