Phase Relations in the FeO-Fe<sub>3</sub>C-Fe<sub>3</sub>N System at 7.8 GPa and 1350 °C: Implications for Oxidation of Native Iron at 250 km

Phase Relations in the FeO-Fe<sub>3</sub>C-Fe<sub>3</sub>N System at 7.8 GPa and 1350 °C: Implications for Oxidation of Native Iron at 250 km

Oxidation of native iron in the mantle at a depth about 250 km and its influence on the stability of main carbon and nitrogen hosts have been reconstructed from the isothermal section of the ternary phase diagram for the FeO-Fe<sub>3</sub>C-Fe<sub>3</sub>N system. The results...

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Bibliographic Details
Main Authors: Aleksei N. Kruk, Alexander G. Sokol, Yurii V. Seryotkin, Yuri N. Palyanov
Format: Article
Language:English
Published: MDPI AG 2020-11-01
Series:Minerals
Subjects:
metal-saturated mantle
high-pressure experiments
oxidation
iron carbide
iron nitride
metal inclusions in diamond
Online Access:https://www.mdpi.com/2075-163X/10/11/984

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https://www.mdpi.com/2075-163X/10/11/984

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