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Evidence for oxygenation of Fe-Mg oxides at mid-mantle conditions and the rise of deep oxygen
As the reaction product of subducted water and the iron core, FeO(2) with more oxygen than hematite (Fe(2)O(3)) has been recently recognized as an important component in the D” layer just above the Earth's core-mantle boundary. Here, we report a new oxygen-excess phase (Mg, Fe)(2)O(3+)(δ) (0 &l...
| Autores principales: | , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Oxford University Press
2020
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8288346/ https://www.ncbi.nlm.nih.gov/pubmed/34691604 http://dx.doi.org/10.1093/nsr/nwaa096 |