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Solid-liquid density and spin crossovers in (Mg, Fe)O system at deep mantle conditions
The low/ultralow-velocity zones in the Earth’s mantle can be explained by the presence of partial melting, critically depending on density contrast between the melt and surrounding solid mantle. Here, first-principles molecular dynamics simulations of (Mg, Fe) O ferropericlase in the solid and liqui...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group
2016
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5118715/ https://www.ncbi.nlm.nih.gov/pubmed/27872491 http://dx.doi.org/10.1038/srep37269 |