Grain-size-sensitive seismic wave attenuation in polycrystalline olivine
In order to investigate the processes responsible for the attenuation of seismic shear waves in the Earth's upper mantle, four olivine polycrystals ranging in mean grain size d from 3 to 23 μm have been fabricated, characterized, and mechanically tested
|Collections||ANU Research Publications|
|Source:||Journal of Geophysical Research|
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