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...

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Detalles Bibliográficos
Autores principales: Cordier, Patrick, Gouriet, Karine, Weidner, Timmo, Van Orman, James, Castelnau, Olivier, Jackson, Jennifer M., Carrez, Philippe
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
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

Internet

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

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