Materials synthesis at terapascal static pressures
Stability of Fe2 S and Fe12 S7 to 125 GPa; implications for S-richplanetary cores
Deformation of Polycrystalline MgO Up to 8.3 GPa and 1270 K: Microstructures, Dominant Slip-Systems, and Transition to Grain Boundary Sliding
Insight into Contact Forces in Crushable Sand using Experiments and Predictive Particle-Scale Modeling
