Seismic anisotropy of the D″ layer induced by (001) deformation of post-perovskite.

ABSTRACT: Crystallographic preferred orientation (CPO) of post-perovskite (Mg,Fe)SiO₃ (pPv) has been believed to be one potential source of the seismic anisotropic layer at the bottom of the lower mantle (D″ layer). However, the natural CPO of pPv remains ambiguous in the D″ layer. Here we have carried out the deformation experiments of pPv-(Mg_0.75,Fe_0.25)SiO₃ using synchrotron radial X-ray diffraction in a membrane-driven laser-heated diamond anvil cell from 135 GPa and 2,500 K to 154 GPa and 3,000 K. Our results show that the intrinsic texture of pPv-(Mg_0.75,Fe_0.25)SiO₃ should be (001) at realistic P-T conditions of the D″ layer, which can produce a shear wave splitting anisotropy of ∼3.7% with V_SH>V_SV

SUBMITTER: Wu X 

PROVIDER: S-EPMC5501973 | biostudies-literature | 2017 Apr

REPOSITORIES: biostudies-literature