1. Dislocation interactions in olivine control postseismic creep of the upper mantle
- Author
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Angus J. Wilkinson, Lars N. Hansen, Ricardo A. Lebensohn, David Wallis, Wallis, David [0000-0001-9212-3734], Apollo - University of Cambridge Repository, Wilkinson, Angus J [0000-0002-8801-4102], Lebensohn, Ricardo A [0000-0002-3152-9105], Wilkinson, Angus J. [0000-0002-8801-4102], and Lebensohn, Ricardo A. [0000-0002-3152-9105]
- Subjects
147/135 ,010504 meteorology & atmospheric sciences ,EarthArXiv|Physical Sciences and Mathematics|Physics ,General Physics and Astronomy ,3705 Geology ,EarthArXiv|Physical Sciences and Mathematics|Earth Sciences ,010502 geochemistry & geophysics ,704/4111 ,01 natural sciences ,bepress|Physical Sciences and Mathematics|Physics|Condensed Matter Physics ,Viscosity ,EarthArXiv|Physical Sciences and Mathematics|Earth Sciences|Mineral Physics ,Seismology ,Condensed Matter - Materials Science ,Multidisciplinary ,EarthArXiv|Physical Sciences and Mathematics|Earth Sciences|Geology ,Deformation (mechanics) ,article ,Mechanics ,Geophysics ,Creep ,704/2151/508 ,Dislocation ,3706 Geophysics ,bepress|Physical Sciences and Mathematics ,Materials science ,bepress|Physical Sciences and Mathematics|Physics ,Science ,147 ,bepress|Physical Sciences and Mathematics|Earth Sciences|Tectonics and Structure ,bepress|Physical Sciences and Mathematics|Earth Sciences ,FOS: Physical sciences ,engineering.material ,General Biochemistry, Genetics and Molecular Biology ,Mantle (geology) ,bepress|Physical Sciences and Mathematics|Earth Sciences|Mineral Physics ,Stress (mechanics) ,0105 earth and related environmental sciences ,Olivine ,bepress|Physical Sciences and Mathematics|Earth Sciences|Geology ,Natural hazards ,Materials Science (cond-mat.mtrl-sci) ,37 Earth Sciences ,General Chemistry ,Strain hardening exponent ,EarthArXiv|Physical Sciences and Mathematics|Physics|Condensed Matter Physics ,EarthArXiv|Physical Sciences and Mathematics ,3703 Geochemistry ,13. Climate action ,704/2151/2809 ,EarthArXiv|Physical Sciences and Mathematics|Earth Sciences|Tectonics and Structure ,engineering - Abstract
Changes in stress applied to mantle rocks, such as those imposed by earthquakes, induce a period of evolution in viscosity and microstructure. This transient creep is often modelled based on stress transfer among slip systems due to grain interactions. However, recent experiments have demonstrated that the intragranular accumulation of stresses among dislocations is the dominant cause of strain hardening in olivine at low temperatures, raising the question of whether the same process contributes to transient creep at higher temperatures. Here, we demonstrate that olivine samples deformed at 25{\deg}C or 1150 to 1250{\deg}C both contain stress heterogeneities of ~1 GPa that are imparted by dislocations and have correlation lengths of ~1 micrometre. The similar stress distributions formed in both temperature regimes indicate that accumulation of stresses among dislocations also provides a contribution to transient creep at high temperatures. The results motivate a new generation of models that capture these intragranular processes and may refine predictions of evolving mantle viscosity over the earthquake cycle., Comment: 17 pages, 5 figures, 2 tables
- Published
- 2021