Grain misorientations in partially molten olivine aggregates: an electron backscatter diffraction study
In polycrystalline aggregates of olivine with mean grain sizes above 35 μm plus a low basaltic melt fraction, both wetted and melt-free grain boundaries are observed after equilibration times at high pressures and temperatures of between 15 and 25 days.
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|Source:||Physics and Chemistry of Minerals|
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