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)DOI: info:10.1007/s00410-022-01933-6v. 177No. 7Springer
Davis, Fred A. and Cottrell, Elizabeth. 2022. "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)." Contributions to Mineralogy and Petrology, 177, (7). https://doi.org/10.1007/s00410-022-01933-6.