Correction to: Partitioning of Fe2O3 in peridotite partial melting experiments over a range of oxygen fugacities elucidates ferric iron systematics in mid-ocean ridge basalts and ferric iron content of the upper mantle

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作者：

Fred A. Davis

Elizabeth Cottrell

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[1] University of Minnesota Duluth,Department of Earth and Environmental Sciences

[2] Smithsonian Institution,National Museum of Natural History

来源：

Contributions to Mineralogy and Petrology | 2022年 / 177卷

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[1] Partitioning of Fe2O3 in peridotite partial melting experiments over a range of oxygen fugacities elucidates ferric iron systematics in mid-ocean ridge basalts and ferric iron content of the upper mantle
Fred A. Davis
Elizabeth Cottrell
Contributions to Mineralogy and Petrology, 2021, 176
[2] Partitioning of Fe2O3 in peridotite partial melting experiments over a range of oxygen fugacities elucidates ferric iron systematics in mid-ocean ridge basalts and ferric iron content of the upper mantle
Davis, Fred A.
Cottrell, Elizabeth
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 2021, 176 (09)
[3] Partitioning of Fe2O3 in peridotite partial melting experiments over a range of oxygen fugacities elucidates ferric iron systematics in mid-ocean ridge basalts and ferric iron content of the upper mantle (vol 176, 67, 2021)
Davis, Fred A.
Cottrell, Elizabeth
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 2022, 177 (07)