Crystallographic preferred orientation of akimotoite and seismic anisotropy of Tonga slab

Rei Shiraishi, Eiji Ohtani, Kyuichi Kanagawa, Akira Shimojuku, Dapeng Zhao

Research output: Contribution to journalArticlepeer-review

24 Citations (Scopus)


The mineral akimotoite, ilmenite-structured MgSiO3, exists at the bottom of the Earth'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. It has been predicted that if akimotoite crystals are preferentially oriented by plastic deformation, a cold subducted slab would be extremely anisotropic. However, there have been no studies of crystallographic preferred orientations and very few reports of plastic deformation experiments for MgSiO3 ilmenite. Here we present plastic deformation experiments on polycrystalline akimotoite, which were conducted at confining pressures of 20-22 GPa and temperatures of 1,000-1,300°C. We found a change in crystallographic preferred orientation pattern of akimotoite with temperature, where the c-axis maximum parallel to the compression direction develops at high temperature, whereas the c axes are preferentially oriented parallel to the shear direction or perpendicular to the compression direction at lower temperature. The previously reported difference in compressional-wave seismic anisotropy between the northern and southern segments of the Tonga slab at depths of the mantle transition zone can conceivably be attributed to the difference in the crystallographic preferred orientation pattern of akimotoite at varying temperature within the slab.

Original languageEnglish
Pages (from-to)657-660
Number of pages4
Issue number7213
Publication statusPublished - 2008 Oct 2


Dive into the research topics of 'Crystallographic preferred orientation of akimotoite and seismic anisotropy of Tonga slab'. Together they form a unique fingerprint.

Cite this