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The
relation between lattice preferred orientation and flow
geometry or stress orientation must be investigated under
a wide range of physical conditions. The results will have
important applications to the interpretation of seismic
anisotropy and the mechanisms of shear localization.
U.S. National Report to IUGG, 1991-1994
Rev. Geophys. Vol. 33
Suppl., © 1995 American Geophysical Union