Low‐Temperature (100°C–300°C) Magnetite Production in Variably Serpentinized Lherzolites
Abstract The study of the serpentinization process in ultramafic rocks has been revived in recent years in response to the problems of natural hydrogen generation. Serpentinization results in the formation of magnetite, which is often observed in the most serpentinized peridotites, at concentrations...
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| Autors principals: | , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Wiley
2025-10-01
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| Col·lecció: | Geochemistry, Geophysics, Geosystems |
| Matèries: | |
| Accés en línia: | https://doi.org/10.1029/2024GC012127 |
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