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Nature ${rb.getVolume()}, 657-660 (2 October 2008) | doi:10.1038/nature07301;
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Crystallographic preferred orientation of akimotoite and seismic anisotropy of Tonga slab
The mineral akimotoite, ilmenite-structured MgSiO3, exists at the bottom of the Earth|[rsquo]|s mantle transition zone and within the uppermost lower mantle, especially under low-temperature conditions. Akimotoite is thought to be a major constituent of the harzburgite layer of subducting slabs, and the most anisotropic mineral in the mantle transition zone.
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