Avoid common mistakes on your manuscript.
Correction to: Contributions to Mineralogy and Petrology (2021) 176:67 https://doi.org/10.1007/s00410-021-01823-3
-
1.
Published Eq. (2) contains a typo. The correct version of Eq. (2) should be:
$${\ln(D}_{\text{Fe}2\text{O}3}^{\text{spl}/\text{melt}})=a\frac{10000}{T}+b+c\ln({C}_{\text{Fe}2\text{O}3}^{\text{spl}})$$(2)where T is temperature in Kelvin and \({C}_{\text{Fe}2\text{O}3}^{\text{spl}}\) is wt.% of Fe2O3 in spinel. Fits are a = 0.87 ± 0.07, b = − 4.6 ± 0.4, and c = 0.24 ± 0.02. We used the correct version of the equation in all our calculations, models, and figures; our results, discussion, and conclusions remain unchanged.
-
2.
We did not provide the duration of the piston cylinder experiments. Each experiment had a run duration of 24 h after reaching the run temperature.
-
3.
In the abstract, the line beginning, “If we allow \({D}_{\text{Fe}2\text{O}3}^{\text{opx}/\text{melt}}\) and \({D}_{\text{Fe}2\text{O}3}^{\text{opx}/\text{melt}}\) to also vary with temperature…” should instead be, “If we allow \({D}_{\text{Fe}2\text{O}3}^{\text{opx}/\text{melt}}\) and \({D}_{\text{Fe}2\text{O}3}^{\text{cpx}/\text{melt}}\) to also vary with temperature…”
-
4.
The green and orange lines in Fig. 9 are mineral/melt partition coefficients estimated by Mallmann and O’Neill (2009) for \({D}_{\text{Fe}2\text{O}3}^{\text{cpx}/\text{melt}}\) and \({D}_{\text{Fe}2\text{O}3}^{\text{opx}/\text{melt}}\), respectively.
Reference
Mallmann G, O’Neill HSC (2009) The crystal/melt partitioning of V during mantle melting as a function of oxygen fugacity compared with some other elements (Al, P, Ca, Sc, Ti, Cr, Fe, Ga, Y, Zr and Nb). J Petrol 50:1765–1794
Author information
Authors and Affiliations
Corresponding author
Additional information
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Rights and permissions
Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
About this article
Cite this article
Davis, F.A., Cottrell, E. 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. Contrib Mineral Petrol 177, 68 (2022). https://doi.org/10.1007/s00410-022-01933-6
Published:
DOI: https://doi.org/10.1007/s00410-022-01933-6