Active conversion of atmospheric carbon dioxide to methane in peridotites of the Samail Ophiolite, Oman
Abstract Methane (CH $${}_{4}$$ ) is common in fluids sourced from low-temperature hydrating (serpentinizing) peridotites, but the carbon sources, rates, and mechanisms of CH $${}_{4}$$ formation are uncertain. In CH $${}_{4}$$ dissolved in groundwaters pumped from four wells of up to 400 m depth in...
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| Principais autores: | , , , , |
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| Format: | Artigo |
| Jezik: | Inglês |
| Izdano: |
Nature Portfolio
2026-01-01
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| Serija: | Scientific Reports |
| Online dostop: | https://doi.org/10.1038/s41598-025-34170-5 |
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