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

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© The Author(s) 2026

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Fig. 2 — A schematic geologic map of the study area including the Kempirsai ultramafic massif and the surrounding sedimentary and igneous terrains of the Mugozhdar zone and Mugozhdar microcontinent. The Bogestay–Kenoy region (on the right) in the southeastern part of the study area is characterized by the extensive occurrence of SCD’s. A-B shows the location of the geological cross-section displayed in Fig. 14.