Abstract: First principles determination of the dissociation boundary of phase H (MgSiO<sub>4</sub>H<sub>2</sub>) and possible existence of ice VII at lower mantle conditions. (AGU Fall Meeting 2018)

First principles determination of the dissociation boundary of phase H (MgSiO₄H₂) and possible existence of ice VII at lower mantle conditions.

Jun Tsuchiya, Ehime University, Geodynamics Research Center, Matsuyama, Japan and Koichiro Umemoto, Tokyo Institute of Technology, Earth-Life Science Institute, Tokyo, Japan

Back to: Geophysical Signals of Volatiles, Melting, and Thermochemical Heterogeneity II Posters

First principles determination of the dissociation boundary of phase H (MgSiO4H2) and possible existence of ice VII at lower mantle conditions.

First principles determination of the dissociation boundary of phase H (MgSiO₄H₂) and possible existence of ice VII at lower mantle conditions.