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Melting and defect transitions in FeO up to pressures of Earth’s core-mantle boundary
The high-pressure melting curve of FeO controls key aspects of Earth’s deep interior and the evolution of rocky planets more broadly. However, existing melting studies on wüstite were conducted across a limited pressure range and exhibit substantial disagreement. Here we use an in-situ dual-techniqu...
| 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/PMC10643405/ https://www.ncbi.nlm.nih.gov/pubmed/37957142 http://dx.doi.org/10.1038/s41467-023-43154-w |