Correction to: Nature Communications https://doi.org/10.1038/s41467-024-53508-7, published online 30 October 2024
The original version of this Article contained an error in the Abstract, which incorrectly read ‘Ophiolites, mostly formed via subduction initiation at proto-forearcs, exhibit a unique variation of mantle-derived magmatism from MORB-like to low-Ti tholeiitic and bainitic-like affinities.’ The correct version states ‘Ophiolites, mostly formed via subduction initiation at proto-forearcs, exhibit a unique variation of mantle-derived magmatism from MORB-like to low-Ti tholeiitic and boninitic-like affinities’. This has been corrected in both the PDF and HTML versions of the Article.
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Zhang, PF., Zhou, MF., Robinson, P.T. et al. Publisher Correction: Diversities of chromite mineralization induced by chemo–thermal evolution of the mantle during subduction initiation. Nat Commun 15, 10004 (2024). https://doi.org/10.1038/s41467-024-54563-w
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DOI: https://doi.org/10.1038/s41467-024-54563-w
