Crystallographic preferred orientations and misorientations in some olivine rocks deformed by diffusion or dislocation creep.
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Fliervoet, T
Drury, Martyn
Chopra, Prame
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Elsevier
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The development of crystallographic preferred orientations (CPO) and grain misorientation distributions (MOD) in fine-grained (0.5-30 μm) olivine rocks, experimentally deformed by diffusion creep and dislocation creep has been investigated. The use of el
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Tectonophysics
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2037-12-31
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