The Mg-carbonate–Fe interaction: Implication for the fate of subducted carbonates and formation of diamond in the lower mantle › Research Explorer

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The Mg-carbonate–Fe interaction: Implication for the fate of subducted carbonates and formation of diamond in the lower mantle

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

Laboratory for Experimental Geochemistry and Petrology of the Earth's Mantle

DOI

https://doi.org/10.1016/j.gsf.2018.10.003
Final published version

Naira S. Martirosyan
Konstantin D. Litasov
Sergey S. Lobanov
Alexander F. Goncharov
Anton Shatskiy
Hiroaki Ohfuji
Vitali Prakapenka

Original language	English
Pages (from-to)	1449-1458
Number of pages	10
Journal	Geoscience Frontiers
Volume	10
Issue number	4
DOIs	https://doi.org/10.1016/j.gsf.2018.10.003
Publication status	Published - 1 Jul 2019

Research areas

Carbide, Carbonate, Deep carbon cycle, High pressure, Iron, Redox reaction, SYSTEM, HIGH-PRESSURE, DEEP LOWER MANTLE, EARTHS MANTLE, IRON-CARBIDE, STABILITY, DIFFRACTION DATA, EQUATION-OF-STATE, TRANSITION ZONE, PHASE-RELATIONS

OECD FOS+WOS

ID: 17288424