Atomistic Mechanism of Al Substitution Effects on the Ferroelastic Post-stishovite Transition by High-Pressure Single-Crystal X-Ray Diffraction

Hydrogen incorporation mechanism in the lower-mantle bridgmanite

Single-crystal X-ray diffraction on the structure of (Al,Fe)-bearing bridgmanite in the lower mantle

Single-crystal elasticity of (Al,Fe)-bearing bridgmanite up to 82 GPa

Atomistic insight into the ferroelastic post-stishovite transition by high-pressure single-crystal X-ray diffraction

High-pressure experimental study of tetragonal CaSiO 3 -perovskite to 200 GPa

Single-crystal elasticity of phase Egg AlSiO 3 OH and δ-AlOOH by Brillouin spectroscopy

Nonlinear effects of hydration on high-pressure sound velocities of rhyolitic glasses

Elasticity of single-crystal Fe-enriched diopside at high-pressure conditions: Implications for the origin of upper mantle low-velocity zones

Elasticity of single-crystal periclase at high pressure and temperature: The effect of iron on the elasticity and seismic parameters of ferropericlase in the lower mantle

Feldspar Raman shift and application as a magmatic thermobarometer

Iron partitioning in natural lower-mantle minerals: Toward a chemically heterogeneous lower mantle

Equation of state and hyperfine parameters of high-spin bridgmanite in the Earth’s lower mantle by synchrotron X-ray diffraction and Mössbauer spectroscopy

Determination of the full elastic tensor of single crystals using shear wave velocities by Brillouin spectroscopy

Synthesis of large and homogeneous single crystals of water-bearing minerals by slow cooling at deep-mantle pressures

Spin and valence states of iron in Al-bearing silicate glass at high pressures studied by synchrotron Mössbauer and X-ray emission spectroscopy

Thermal equation of state and spin transition of magnesiosiderite at high pressure and temperature

Spin transition of Fe 2+ in ringwoodite (Mg,Fe) 2 SiO 4 at high pressures

Synchrotron Mössbauer study of Fe-bearing pyrope at high pressures and temperatures

Magnesite formation from MgO and CO 2 at the pressures and temperatures of Earth’s mantle