The effect of temperature on the seismic anisotropy of the perovskite and post-perovskite polymorphs of MgSiO 3

By S. Stackhouse, J. Brodholt, J. Wookey, J. Kendall, G. D. Price. 2004

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Postperovskite phase transition and its geophysical implications (2006, background): “The elastic properties were calculated both at 0 K [Tsuchiya et al., 2004b; Iitaka et al., 2004; Oganov and Ono, 2004] and high temperatures [Stackhouse et al., 2005; Wookey et al., 2005; Wentzcovitch et al., 2006].”
Dynamics and evolution of the deep mantle resulting from thermal, chemical, phase and melting effects (2012, background): “The mechanical properties of pPv, including seismic velocity and viscosity, are strongly anisotropic due to its crystal structure (Stackhouse et al., 2005; Wentzcovitch et al., 2006).”
Shear Wave Splitting and Mantle Anisotropy: Measurements, Interpretations, and New Directions (2009, background): “The single-crystal elasticity of postperovskite is not yet well understood; several different sets of elastic constants obtained from first-principles calculations have been published (Iitaka et al. 2004; Stackhouse et al. 2005; Wentzcovitch et al. 2006) but discrepancies among studies exist.”