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Viscosity of hcp iron at Earth’s inner core conditions from density functional theory
The inner core, extending to 1,221 km above the Earth’s center at pressures between 329 and 364 GPa, is primarily composed of solid iron. Its rheological properties influence both the Earth’s rotation and deformation of the inner core which is a potential source of the observed seismic anisotropy. H...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2020
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7156496/ https://www.ncbi.nlm.nih.gov/pubmed/32286388 http://dx.doi.org/10.1038/s41598-020-63166-6 |