Phase relations in the Fe-Fe3C-Fe3N system at 7.8 GPa and 1350 °C › Research Explorer

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Phase relations in the Fe-Fe₃C-Fe₃N system at 7.8 GPa and 1350 °C: Implications for carbon and nitrogen hosts in Fe⁰-saturated upper mantle

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

Ultrahigh Pressure Mineralogy Laboratory

DOI

https://doi.org/10.1016/j.pepi.2017.02.007
Final published version

Alexander G. Sokol
Alexey N. Kruk
Yurii V. Seryotkin
Alexander A. Korablin
Yury N. Palyanov

Original language	English
Pages (from-to)	43-53
Number of pages	11
Journal	Physics of the Earth and Planetary Interiors
Volume	265
DOIs	https://doi.org/10.1016/j.pepi.2017.02.007
Publication status	Published - 1 Apr 2017

Research areas

OXYGEN FUGACITY, HIGH-PRESSURE, PERIDOTITE XENOLITHS, THERMAL-EXPANSION, DIAMOND FORMATION, IRON CARBIDE, NOBLE-GASES, INCLUSIONS, GRAPHITE, SILICATE

OECD FOS+WOS

ID: 10036210