High-pressure minerals

Stability, composition, and crystal structure of Fe-bearing Phase E in the transition zone

Discovery of asimowite, the Fe-analog of wadsleyite, in shock-melted silicate droplets of the Suizhou L6 and the Quebrada Chimborazo 001 CB3.0 chondrites

Phase transition of wadsleyite-ringwoodite in the Mg 2 SiO 4 -Fe 2 SiO 4 system

Decomposition boundary from high-pressure clinoenstatite to wadsleyite + stishovite in MgSiO 3

X-ray single-crystal structural characterization of Na 2 MgSiO 4 with cristobalite-type structure synthesised at 22 GPa and 1800 °C

Chromium-bearing phases in the Earth's mantle: Evidence from experiments in the Mg 2 SiO 4 –MgCr 2 O 4 system at 10–24 GPa and 1600°C

The equation of state of wadsleyite solid solutions: Constraining the effects of anisotropy and crystal chemistry

Experimental and thermodynamic investigations on the stability of Mg 14 Si 5 O 24 anhydrous phase B with relevance to Mg 2 SiO 4 forsterite, wadsleyite, and ringwoodite

Majorite-olivine–high-Ca pyroxene assemblage in the shock-melt veins of Pervomaisky L6 chondrite

Transition metals in the transition zone: Crystal chemistry of minor element substitution in wadsleyite

Modeling dislocation glide and lattice friction in Mg 2 SiO 4 wadsleyite in conditions of the Earth’s transition zone

Coupled substitution of Fe 3+ and H + for Si in wadsleyite: A study by polarized infrared and Mössbauer spectroscopies and single-crystal X-ray diffraction

(FeH) 1−x Ti x O 2 : A new water carrier to the mantle transition zone

Dislocation microstructures in simple-shear-deformed wadsleyite at transition-zone conditions: Weak-beam dark-field TEM characterization of dislocations on the (010) plane

Synthesis of large wadsleyite single crystals by solid-state recrystallization

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

Structural and chemical characterization of Mg[(Cr,Mg)(Si,Mg)]O 4 , a new post-spinel phase with sixfold-coordinated silicon

Synthesis of a quenchable high-pressure form of magnetite (h-Fe 3 O 4 ) with composition Fe1 (Fe 2+ 0.75 Mg 0.26 ) Fe2 (Fe 3+ 0.70 Cr 0.15 Al 0.11 Si 0.04 ) 2 O 4

In-situ infrared spectra of hydroxyl in wadsleyite and ringwoodite at high pressure and high temperature