A critical evaluation of pressure scales at high temperatures by in situ X-ray diffraction measurements

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Unified analyses for P-V-T equation of state of MgO: A solution for pressure-scale problems in high P-T experiments (2008, methodology): “[5] Previously proposed several pressure scales were made by using experimental data measured depending on other pressure scales [e.g., Shim et al., 2002; Fei et al., 2004a; Hirose et al., 2008].”
Experimentally determined postspinel transformation boundary in Mg2SiO4 using MgO as an internal pressure standard and its geophysical implications (2004, unknown): “…of the phase boundaries (compare Figures 4 and 5) because the existing equations of state of pressure standards (Au, MgO, and Pt) predict pressures that can differ by as much as 3 GPa at conditions corresponding to the 660-km seismic discontinuity [e.g., Shim et al., 2002; Fei et al., 2003].”
Spin state of ferric iron in MgSiO3 perovskite and its effect on elastic properties (2010, unknown): “pressure (Shim et al., 2001a; Fei et al., 2004).”