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. 2024 Nov 19;15:10004. doi: 10.1038/s41467-024-54563-w

Publisher Correction: Diversities of chromite mineralization induced by chemo–thermal evolution of the mantle during subduction initiation

Peng-Fei Zhang 1,, Mei-Fu Zhou 1,, Paul T Robinson 1, John Malpas 2, Graciano P Yumul Jr 3, Christina Yan Wang 4, Jie Li 5
PMCID: PMC11576726  PMID: 39562562

Correction to: Nature Communications 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.

Contributor Information

Peng-Fei Zhang, Email: zhangpengfei073061@163.com.

Mei-Fu Zhou, Email: zhoumeifu@hotmail.com.


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