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Quaternary low-temperature serpentinization and carbonation in the New Caledonia ophiolite
The low-temperature alteration (< 150 °C) of ophiolites by infiltrated meteoric waters removes atmospheric CO(2) through mineral carbonation and is assumed to generate H(2) and possibly CH(4) according to so-called serpentinization reactions. This overall alteration pattern is primarily constrain...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2023
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10632469/ https://www.ncbi.nlm.nih.gov/pubmed/37940638 http://dx.doi.org/10.1038/s41598-023-46691-y |