High-pressure phase transition of olivine-type Mg 2 GeO 4 to a metastable forsterite-III type structure and their equations of state

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

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

Structure and titanium distribution of feiite characterized using synchrotron single-crystal X-ray diffraction techniques

Thermal equation of state of ice-VII revisited by single-crystal X-ray diffraction

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

Hydrogen solubility in FeSi alloy phases at high pressures and temperatures

Pressure-induced C 23– C 37 transition and compression behavior of orthorhombic Fe 2 S to Earth’s core pressures and high temperatures

A multi-faceted experimental study on the dynamic behavior of MgSiO 3 glass in the Earth’s deep interior

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

A high-pressure, clinopyroxene-structured polymorph of albite in highly shocked terrestrial and meteoritic rocks

Elasticity and high-pressure behavior of Mg 2 Cr 2 O 5 and CaTi 2 O 4 -type phases of magnesiochromite and chromite

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

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

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

Stöfflerite, (Ca,Na)(Si,Al) 4 O 8 in the hollandite structure: A new high-pressure polymorph of anorthite from martian meteorite NWA 856

Phase transitions in ε-FeOOH at high pressure and ambient temperature

Thermal equation of state of post-aragonite CaCO3-Pmmn

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

Chenmingite, FeCr 2 O 4 in the CaFe 2 O 4 -type structure, a shock-induced, high-pressure mineral in the Tissint martian meteorite