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Sequestration of Martian CO(2) by mineral carbonation
Carbonation is the water-mediated replacement of silicate minerals, such as olivine, by carbonate, and is commonplace in the Earth’s crust. This reaction can remove significant quantities of CO(2) from the atmosphere and store it over geological timescales. Here we present the first direct evidence...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Pub. Group
2013
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4354006/ https://www.ncbi.nlm.nih.gov/pubmed/24149494 http://dx.doi.org/10.1038/ncomms3662 |