Shear deformation experiments of forsterite at 11 Gpa - 1400°C in the multianvil apparatus

By H. Couvy, D. Frost, F. Heidelbach, K. Nyilas, T. Ungár, S. Mackwell, P. Cordier. 2004

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Geodynamic Significance of Seismic Anisotropy of the Upper Mantle: New Insights from Laboratory Studies (2008, background): “Second, Couvy et al. (2004) reported that olivine LPO at high pressures is different from that at lower pressures, and they proposed that pressure might change olivine LPO (see also Raterron et al. 2007, Mainprice et al. 2005).”
Shear Wave Splitting and Mantle Anisotropy: Measurements, Interpretations, and New Directions (2009, background): “, Keith and Crampin (1977), Kosarev et al.”
Upper mantle seismic anisotropy resulting from pressure-induced slip transition in olivine (2009, background): “Further experimentation at high pressure and theoretical calculations, however, have complicated the issue by finding the same switch in the olivine easy-slip direction (from [100] to [001]) in a dry environment at pressures in excess of 3 GPa (refs&nbs”
Effect of water and stress on the lattice-preferred orientation of olivine (2006, background): “Indeed, Couvy et al. (2004) recently suggested that the pressure may have an intrinsic effect to enhance the activity of the b=[001] slip systems relative to the b=[100] slip systems.”