Transient Creep in Subduction Zones by Long‐Range Dislocation Interactions in Olivine
Author:
Affiliation:
1. Department of Earth Sciences University of Cambridge Cambridge UK
2. Department of Earth Sciences Utrecht University Utrecht The Netherlands
3. Department of Earth and Environmental Sciences University of Minnesota Minneapolis MN USA
Funder
Natural Environment Research Council
Aard- en Levenswetenschappen, Nederlandse Organisatie voor Wetenschappelijk Onderzoek
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB022618
Reference87 articles.
1. The elastic constants of San Carlos olivine to 17 GPa
2. Plate interface rheological switches during subduction infancy: Control on slab penetration and metamorphic sole formation
3. Controls on the rheological properties of peridotite at a palaeosubduction interface: A transect across the base of the Oman–UAE ophiolite
4. On the viscous flow in metals, and allied phenomena
5. The creep of polycrystalline ice
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3. Modeling diffusion in ionic, crystalline solids with internal stress gradients;Geochimica et Cosmochimica Acta;2023-08
4. Dislocation and disclination densities in experimentally deformed polycrystalline olivine;European Journal of Mineralogy;2023-03-31
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