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. 2026 Jan 17;16:2613. doi: 10.1038/s41598-025-33781-2

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© The Author(s) 2026

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 licence, and indicate if changes were made. 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/4.0/.

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Fig. 2 — (a) Serpentinite rocks were thrusted over the metavolcanics along NE trend, (b) Close up view of pale gray talc carbonates, (c) Highly weathered granodiorite showing monumental shapes intruded the metavolcanics, (d) Quartz vein invaded the monzogranite along NE trend, (e) Sharp intrusive contact between the monzogranite and the metavolcanics, (f) Monzogranite intrudes the granodiorite.