Experimental deformation of forsterite, wadsleyite and ringwoodite: Implications for seismic anisotropy of the Earth's mantle
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![Figure 1 Preferred orientation of [100], [010] and [001] crystallographic axes in synthetic olivine polycrystal S2954 deformed at 1,400 8 C and 11 GPa confining pressure in simple shear 9](https://thumb-eu.123doks.com/thumbv2/123doknet/14664530.740428/160.892.462.833.879.1023/preferred-orientation-crystallographic-synthetic-polycrystal-deformed-confining-pressure.webp)
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