2020, Hernandez, J.-A., Morard, G., Guarguaglini, M., Alonso-Mori, R., Benuzzi-Mounaix, A., Bolis, R., Fiquet, G., Galtier, E., Gleason, A.E., Glenzer, S., Guyot, F., Ko, B., Lee, H.J., Mao, W.L., Nagler, B., Ozaki, N., Schuster, A.K., Shim, S.H., Vinci, T., Ravasio, A.

We report in situ structural measurements of shock-compressed single crystal orthoenstatite up to 337 ± 55 GPa on the Hugoniot, obtained by coupling ultrafast X-ray diffraction to laser-driven shock compression. Shock compression induces a disordering of the crystalline structure evidenced by the appearance of a diffuse X-ray diffraction signal at nanosecond timescales at 80 ± 13 GPa on the Hugoniot, well below the equilibrium melting pressure (>170 GPa). The formation of bridgmanite and post-perovskite have been indirectly reported in microsecond-scale plate-impact experiments. Therefore, we interpret the high-pressure disordered state we observed at nanosecond scale as an intermediate structure from which bridgmanite and post-perovskite crystallize at longer timescales. This evidence of a disordered structure of MgSiO3 on the Hugoniot indicates that the degree of polymerization of silicates is a key parameter to constrain the actual thermodynamics of shocks in natural environments. © 2020. The Authors.