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An experimental study, implicated in the revealing of the conditions for the origin for Fe3+-bearing magnesiowustite in the lithospheric mantle, was performed using Mossbauer spectroscopy of pre-synthesized samples. Experiments were carried out using a multi-anvil high-pressure split-sphere apparatus at 6.3–7.5 GPa, in the range of 1100–1650 °C in carbonate-metal, carbonate–oxide-metal, carbonate-oxide, carbide-oxide and carbonate–metal- sulphur systems. In three experimental series, oxygen fugacity gradient in the samples was created, which enabled the study of the processes of magnesiowustite formation under oxidizing and reducing conditions (ΔlogfO2 (FMQ) values from −1 to −5). It was established that Fe3+-bearing magnesiowustite can form both in assemblage with oxidized phases, such as carbonate or with reduced ones—metal, carbides, sulphides, graphite and diamond. According to the Mossbauer spectroscopy, the composition of synthesized magnesiowustite varied within a range of Fe3+/ΣFe values from 0 to 0.3, with IV and VI coordination of Fe3+ depending on P, T, fO2, x-parameters. It was established that Fe3+-bearing magnesiowustite formation processes under upper mantle P,T-conditions include redox reactions, with magnesiowustite being (1) reductant or (2) product of interaction, (3) crystallization processes of magnesiowustite from an oxidized melt, where magnesiowustite acts as a sink for ferric iron and (4) iron disproportionation.

Processes and Conditions of the Origin for Fe3+-Bearing Magnesiowüstite under Lithospheric Mantle Pressures and Temperatures