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Direct
experimentation to investigate the creep strengths of high pressure
silicates should be performed. Also, the role of grain-size reduction
on rheology should be investigated through experimental studies on
transformation kinetics and deformation in the grain-size sensitive
regime.
U.S. National Report to IUGG, 1991-1994
Rev. Geophys. Vol. 33
Suppl., © 1995 American Geophysical Union