by | Aug 24, 2022 | vol23

Corrigendum to “Equilibrium olivine-melt Mg isotopic fractionation explains high δ26Mg values in arc lavas” by Liu et al., 2022

X.-N. Liu1,

1School of Earth Science, University of Bristol, Wills Memorial Building, Bristol BS8 1RJ, UK

R.C. Hin1,

1School of Earth Science, University of Bristol, Wills Memorial Building, Bristol BS8 1RJ, UK

C.D. Coath1,

1School of Earth Science, University of Bristol, Wills Memorial Building, Bristol BS8 1RJ, UK

M. van Soest2,

2School of Earth and Space Exploration, ISTB4, Arizona State University, Tempe 85287, AZ, USA

E. Melekhova3,

3Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK

T. Elliott1

1School of Earth Science, University of Bristol, Wills Memorial Building, Bristol BS8 1RJ, UK

Affiliations | Corresponding Author | Cite as

Geochemical Perspectives Letters v23 | https://doi.org/10.7185/geochemlet.2226cor
Received 8 August 2022 | Accepted 11 August 2022 | Published 24 August 2022

Copyright © 2022 The Authors

Published by the European Association of Geochemistry
under Creative Commons License CC BY-NC-ND 4.0

 

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Corrigendum

Corrigendum | Original article

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.



Figure S-6 Long-term variations in the magnesium isotope composition of rock standard BHVO-2, indicating a reproducibility of 0.027 ‰ (2 s.d.).

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