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Periclase deforms more slowly than bridgmanite under mantle conditions
Transport of heat from the interior of the Earth drives convection in the mantle, which involves the deformation of solid rocks over billions of years. The lower mantle of the Earth is mostly composed of iron-bearing bridgmanite MgSiO(3) and approximately 25% volume periclase MgO (also with some iro...
| 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/PMC9834053/ https://www.ncbi.nlm.nih.gov/pubmed/36631648 http://dx.doi.org/10.1038/s41586-022-05410-9 |