Carbon retention during subduction of ophicarbonate rocks from the Zermatt-Saas unit (Western Alps)

Abstract Serpentinite-hosted carbonate rocks (i.e., ophicarbonates) are an important rock type for the deep C cycle because they can occur either in the slab or in the mantle wedge. We present a case study of ophicarbonate rocks from the Zermatt-Saas unit, Western Alps, that were subducted up to ecl...

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Bibliographic Details
Main Authors: Francesca Piccoli, Aaron A. Hutter, Jörg Hermann
Format: Article
Language:English
Published: SpringerOpen 2025-05-01
Series:Swiss Journal of Geosciences
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Online Access:https://doi.org/10.1186/s00015-025-00479-6
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