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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...
Gorde:
| Argitaratua izan da: | Sci Rep |
|---|---|
| Egile Nagusiak: | , |
| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Nature Publishing Group
2016
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| Gaiak: | |
| Sarrera elektronikoa: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5118715/ https://ncbi.nlm.nih.gov/pubmed/27872491 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep37269 |
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