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. 2026 May 27;16:24114. doi: 10.1038/s41598-026-55055-1

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© The Author(s) 2026

Open Access This article is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License, which permits any non-commercial use, sharing, 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 licence, and indicate if you modified the licensed material. You do not have permission under this licence to share adapted material derived from this article or parts of it. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence 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 licence, visit http://creativecommons.org/licenses/by-nc-nd/4.0/.

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Fig. 13 — (A, B) Thin-section microphotographs illustrating the mineralogical and textural features of the ultramafic samples, including the distribution and alteration patterns of serpentine, olivine, pyroxene, and chromite. (C) X-ray diffractogram highlighting the dominant mineral phases and confirming the pervasive serpentinization within the studied rocks. (D) SEM–EDS analyses documenting the microtextural attributes and chemical compositions of the principal ultramafic mineral phases, providing insights into their alteration pathways and element redistribution during serpentinization.