Elastic anisotropy of FeSiO3 end-members of the perovskite and post-perovskite phases

نویسندگان

  • Stephen Stackhouse
  • John P. Brodholt
  • David Price
چکیده

[1] The athermal elastic constants of the perovskite and post-perovskite polymorphs of pure end-member FeSiO3 were calculated from ab initio calculations. We predict that incorporating ten mole percent FeSiO3 together with four mole percent Al2O3 into MgSiO3 reduces the perovskite to post-perovskite phase transition pressure by 5 GPa. Small changes in the seismic properties of the post-perovskite phase due to the incorporation of iron and alumina are compatible with observations for the lower mantle. MgSiO3 post-perovskite enriched in fifty percent or more iron may be responsible for ultra-low velocity zones at the base of the mantle. Citation: Stackhouse, S., J. P. Brodholt, and G. D. Price (2006), Elastic anisotropy of FeSiO3 end-members of the perovskite and post-perovskite phases, Geophys. Res. Lett., 33, L01304, doi:10.1029/2005GL023887.

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تاریخ انتشار 2005