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...
Furkejuvvon:
| Váldodahkkit: | , , |
|---|---|
| Materiálatiipa: | Artigo |
| Giella: | Inglês |
| Almmustuhtton: |
Pensoft Publishers
2025-05-01
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| Ráidu: | Swiss Journal of Geosciences |
| Fáttát: | |
| Liŋkkat: | https://doi.org/10.1186/s00015-025-00479-6 |
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