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Dislocation interactions in olivine control postseismic creep of the upper mantle

Changes in stress applied to mantle rocks, such as those imposed by earthquakes, commonly induce a period of transient creep, which is often modelled based on stress transfer among slip systems due to grain interactions. However, recent experiments have demonstrated that the accumulation of stresses...

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Detalles Bibliográficos
Autores principales: Wallis, David, Hansen, Lars N., Wilkinson, Angus J., Lebensohn, Ricardo A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8190305/
https://www.ncbi.nlm.nih.gov/pubmed/34108476
http://dx.doi.org/10.1038/s41467-021-23633-8