Corrigendum to “Equilibrium olivine-melt Mg isotopic fractionation explains high δ26Mg values in arc lavas” by Liu et al., 2022Affiliations | Corresponding Author | Cite as
1School of Earth Science, University of Bristol, Wills Memorial Building, Bristol BS8 1RJ, UK
2School of Earth and Space Exploration, ISTB4, Arizona State University, Tempe 85287, AZ, USA
3Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK
Liu, X.-N., Hin, R.C., Coath, C.D., van Soest, M., Melekhova, E., Elliott, T. (2022) Corrigendum to “Equilibrium olivine-melt Mg isotopic fractionation explains high δ26Mg values in arc lavas” by Liu et al., 2022. Geochem. Persp. Let. 23, 5–5. https://doi.org/10.7185/geochemlet.2226cor
Correction to: Geochemical Perspectives Letters 22, 42–47, doi: 10.7185/geochemlet.2226, published 19 July 2022.
In Figure S-6 in the Supplementary Information, the δ26Mg value of BHVO-2 was mislabelled as the δ25Mg value of BHVO-2 (−0.103 ± 0.014 ‰, 2 s.d.). The rest of the information in Figure S-6 is correct, including the figure caption. The correct text should be “BHVO-2: −0.202 ± 0.027 ‰ (2 s.d.)”. The figure has now been corrected in the Supplementary Information, and the corrected figure is shown below.