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 mantleDOI: info:10.1007/s00410-021-01823-3v. 176No. 9Springer67–67
Davis, Fred A. and Cottrell, Elizabeth. 2021. "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." Contributions to Mineralogy and Petrology, 176, (9) 67–67. https://doi.org/10.1007/s00410-021-01823-3.