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• W2017658532 abstract "Microstructural analyses of peridotite mylonites from the oceanic lithosphere indicate that shear localization results from the combined effects of grain size reduction, grain boundary sliding and second phase pinning during deformation. The pinning effect, combined with experimental flow laws for olivine, suggests that a permanent transition from dislocation creep processes to diffusion creep occurs. This rheological transition provides a mechanism for long term weakening of the lithosphere for rocks deforming in the brittle–ductile regime. In addition, our results support the hypothesis that a transition to diffusion creep promotes the randomization of pre-existing lattice preferred orientations, which would reduce seismic anisotropy." @default.
• W2017658532 created "2016-06-24" @default.
• W2017658532 creator A5058106939 @default.
• W2017658532 creator A5060121595 @default.
• W2017658532 date "2006-08-01" @default.
• W2017658532 modified "2023-09-27" @default.
• W2017658532 title "Grain size sensitive deformation mechanisms in naturally deformed peridotites" @default.
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• W2017658532 doi "https://doi.org/10.1016/j.epsl.2006.06.006" @default.
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