The reactions between iron and magnesite at 6 GPa and 1273–1873 K: Implication to reduction of subducted carbonate in the deep mantle

  • MARTIROSYAN Naira S.
    Novosibirsk State University V.S. Sobolev Institute of Geology and Mineralogy, SB RAS
  • LITASOV Konstantin D.
    Novosibirsk State University V.S. Sobolev Institute of Geology and Mineralogy, SB RAS
  • SHATSKIY Anton
    Novosibirsk State University V.S. Sobolev Institute of Geology and Mineralogy, SB RAS
  • OHTANI Eiji
    Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University

Abstract

The interaction between Fe–metal and magnesite was studied in multianvil experiments at 6 GPa and 1273–1873 K using different capsule materials: Fe, BN, and MgO. It was observed that at subsolidus conditions reaction proceeds with the formation of Fe3C and magnesiowüstite in the stoichiometric proportions according to relation: MgCO3 + 5Fe = 3(Fe0.66Mg0.33)O + Fe3C. At melting conditions (1673–1873 K) magnesite and iron react in nearly equivalent molar proportions with formation of Mg–Fe–carbonatite melt, Fe–C alloy, magnesiowüstite and graphite. The reactions clearly show that free carbon and metallic iron phases cannot coexist in the upper mantle and presumably in transition zone and will always form Fe–carbide. The carbon content in Fe–C alloy and its coexistence with diamond will be strongly dependent on the oxygen fugacity. The studied reactions can be considered as intermediate processes in the reduced mantle domains at the contact with submerging subduction slabs and have further implication to the processes at the core–mantle boundary.

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Details 詳細情報について

  • CRID
    1390282681521485184
  • NII Article ID
    130005067160
  • DOI
    10.2465/jmps.141003a
  • ISSN
    13493825
    13456296
  • Text Lang
    en
  • Data Source
    • JaLC
    • Crossref
    • CiNii Articles
    • KAKEN
  • Abstract License Flag
    Disallowed

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