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Garnet peridotites reveal spatial and temporal changes in the oxidation potential of subduction
Changes in the oxygen fugacity (fO(2)) of the Earth’s mantle have been proposed to control the spatial and temporal distribution of arc-related ore deposits, and possibly reflect the evolution of the atmosphere over billions of years. Thermodynamic calculations and natural evidence indicate that flu...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2018
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6219559/ https://www.ncbi.nlm.nih.gov/pubmed/30401916 http://dx.doi.org/10.1038/s41598-018-34669-0 |