How is oceanic lithosphere created and modified? Why is the oceanic asthenosphere weak? How is mantle flow recorded within the lithosphere and asthenosphere? What is the scale and vigor of convection beneath the plates?
Seismic anisotropy produced by aligned olivine in oceanic lithosphere offers a window into mid-ocean ridge dynamics. Yet, interpreting anisotropy in the context of grain-scale deformation processes and strain observed in laboratory experiments and …