2021
DOI: 10.1103/physrevlett.126.025701
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Elasticity of a Pseudoproper Ferroelastic Transition from Stishovite to Post-Stishovite at High Pressure

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Cited by 23 publications
(91 citation statements)
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“…Additionally, the Cij00 ${C}_{ij0}^{0}$ can be calculated from literature C ij 0 data of stishovite at ambient conditions after taking into account of the linear Al effect on the C ij 0 in stishovite (Lakshtanov et al., 2007a). Since the pressure‐dependent slopes for Raman shifts and lattice parameters are very similar in Al,H‐bearing and pure SiO 2 stishovite (Figures 2c, 3c, and 3d), the Cij0 ${C}_{ij}^{0}$ slope, the pressure derivatives of Cij0 ${C}_{ij}^{0}$ (Cij0 ${C}_{ij}^{0\prime }$), of the experimentally‐determined values for pure SiO 2 endmember in a recent study can be used for the Al,H‐bearing stishovite (Zhang et al., 2021). The exception here is for the C110 ${C}_{11}^{0\prime }$ and C120 ${C}_{12}^{0\prime }$ that can be affected by the shear softening and the transition pressure such that these two parameters for the Al,H‐bearing stishovite need to be evaluated in the modeling.…”
Section: Discussionmentioning
confidence: 93%
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“…Additionally, the Cij00 ${C}_{ij0}^{0}$ can be calculated from literature C ij 0 data of stishovite at ambient conditions after taking into account of the linear Al effect on the C ij 0 in stishovite (Lakshtanov et al., 2007a). Since the pressure‐dependent slopes for Raman shifts and lattice parameters are very similar in Al,H‐bearing and pure SiO 2 stishovite (Figures 2c, 3c, and 3d), the Cij0 ${C}_{ij}^{0}$ slope, the pressure derivatives of Cij0 ${C}_{ij}^{0}$ (Cij0 ${C}_{ij}^{0\prime }$), of the experimentally‐determined values for pure SiO 2 endmember in a recent study can be used for the Al,H‐bearing stishovite (Zhang et al., 2021). The exception here is for the C110 ${C}_{11}^{0\prime }$ and C120 ${C}_{12}^{0\prime }$ that can be affected by the shear softening and the transition pressure such that these two parameters for the Al,H‐bearing stishovite need to be evaluated in the modeling.…”
Section: Discussionmentioning
confidence: 93%
“…The mineralogy in the selected MORB composition contains 20 vol% stishovite, 30 vol% CF, 30 vol% Bgm, and 20 vol% CaPv in the lower mantle (Ishii et al, 2019). Thermoelastic parameters of these mineral phases, except CaPv, in our modeling are taken from this study, Zhang et al (2021), andXu et al (2008). We should note that Xu et al (2008) determined these parameters using previous elasticity data at high P-T (refer to Table S10 in Supporting Information S1 for details; Akaogi et al, 1999;Fei & Ahrens, 1995;Fiquet et al, 2000;Funamori et al, 1998;Kiefer et al, 2002;Liu et al, 1999;Murakami et al, 2003;Shim & Duffy, 2000;Sinogeikin et al, 2004;Smyth & McCormick, 1995;Wentzcovitch et al, 2004).…”
Section: Velocity Profiles Of Subducted Morb Across the Post-stishovi...mentioning
confidence: 99%
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“…Brillouin scattering measurements were conducted under ambient conditions using a Brillouin Light Scattering (BLS) system at the Mineral Physics Laboratory, the University of Texas at Austin(Fu et al 2017; Fu et al 2019;Zhang et al 2021). In the BLS system, a single-frequency 532 nm solid-state green laser (Coherent Verdi V2) was used as an excitation light source and a JRS six-pass tandem Fabry-Pérot interferometer equipped with a Perkin-Elmer photomultiplier detector was used to record the Brillouin spectra of the sample.…”
mentioning
confidence: 99%