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In a paper just published in Earth and Planetary Science Letters, we combine numerical modeling of dislocation glide with published reults of diffusion experiments and revisit the rheology of wadsleyite, ringwoodite and majorite garnet under geological strain rates across the transition zone of the Earth’s mantle using theoretical plasticity models:

Keynote on "Mechanisms of Ductile Deformation in the Lithospheric Mantle" by Sylvie Demouchy