Experimental Study of Sulfur Solubility in Ca–Mg Carbonate Melt under P–T Parameters of Lithospheric Mantle

Thermal equation of state for zoisite: Implications for the transportation of water into the upper mantle and the high-velocity anomaly in the Farallon plate

A cotunnite-type new high-pressure phase of Fe 2 S

The low-temperature shift of antigorite dehydration in the presence of sodium chloride: In situ diffraction study up to 3 GPa and 700 °C

Synthesis, structure, and single-crystal elasticity of Al-bearing superhydrous phase B

The electrical conductivity of albite feldspar: Implications for oceanic lower crustal sequences and subduction zones

The crystal structure of Fe 2 S at 90 GPa based on single-crystal X-ray diffraction techniques

Synthesis of calcium orthocarbonate, Ca 2 CO 4 - Pnma at P-T conditions of Earth’s transition zone and lower mantle

Peralkalinity in peraluminous granitic pegmatites. II. Evidence from experiments on carbonate formation in spodumene-bearing assemblages

Experimental and Observational Constraints on Halogen Behavior at Depth

Experimental melt inclusion homogenization in a hydrothermal diamond-anvil cell: Comparison with homogenization at one atmosphere

P-V-T measurements of Fe 3 C to 117 GPa and 2100 K: Implications for stability of Fe 3 C phase at core conditions

Deformation and strength of mantle relevant garnets: Implications for the subduction of basaltic-rich crust

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

Probing Phase Transitions and Magnetism in Minerals with Neutrons

High-pressure and high-temperature vibrational properties and anharmonicity of carbonate minerals up to 6 GPa and 500 °C by Raman spectroscopy

P-V-T equation of state of hydrous phase A up to 10.5 GPa

In situ observations of the transition between beryl and phenakite in aqueous solutions using a hydrothermal diamond-anvil cell

Ferric-ferrous iron ratios of experimental majoritic garnet and clinopyroxene as a function of oxygen fugacity

Solubility of Na 2 SO 4 in silica-saturated solutions: Implications for REE mineralization