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. 2022 Sep 14;609(7927):529–534. doi: 10.1038/s41586-022-04981-x

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© The Author(s) 2022

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 license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license 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 license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 2 — a,b, K₂O/TiO₂ versus MgO of the Fagradalsfjall whole-rock samples compared to historical lavas from other ITSCs on the RP^14,17,18 (a) and single-eruptive Icelandic basaltic lavas from different parts of the rift system for which large datasets are available (ref. ³ and references therein) (b). Error bars are included on both panels and include external 2σ error.

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