We study systematically the relationship between olivine lattice preferred orientation and the
mantle flow field that produces it, using the plastic flow/recrystallization model of Kaminski …

The interpretation of seismic anisotropy in the mantle requires a knowledge of the
relationship between the lattice preferred orientation (LPO) of crystals and the convective …

The calculation of the lattice preferred orientation of crystals in mantle flow has become a
major step in the interpretation of the upper mantle seismic anisotropy. Available models for …

Seismic anisotropy in the mantle is primarily due to deformation‐induced lattice preferred
orientation (LPO) of olivine crystals. The aim of this paper is to better understand how such …

The development of Lattice Preferred Orientations (LPO) within olivine aggregates under
flow in the upper mantle leads to seismic and rheological (or viscoplastic) anisotropies. We …

Models of development of lattice preferred orientation (LPO) of crystals aggregates in
convective flow are necessary to interpret the anisotropic seismic signature of the Earth′ s …

Seismic anisotropy in the mantle is primarily caused by the lattice‐preferred orientation
(LPO) of olivine, which forms and evolves in response to progressive plastic deformation …

Flow‐induced mineral alignment in the Earth's mantle affects the nature of seismic wave
propagation. Since measurements of seismic travel time and shear wave splitting are a key …

The anisotropic seismic structure due to flow‐induced mineral alignment is investigated for a
series of models designed to simulate deformation in the upper mantle within a few hundred …

Deformation of peridotite caused by mantle flow beneath an oceanic spreading centre can
result in the development of seismic anisotropy. Traveltime anomalies and shearwave …