Lateral variations of seismic wave speeds and attenuation (dissipation of strain energy) in
the Earth's upper mantle have the potential to map key characteristics such as temperature …

Melt inclusions record the depth of magmatic processes, magma degassing paths, and
volatile budgets of magmas. Extracting this information is a major challenge. It requires …

The rate at which H+ moves into, through, and out of olivine is of great interest for
understanding the deep water cycle, assessing the fidelity of olivine-hosted melt inclusions …

We study the mechanical response and correlated microstructure of axial deformed fine-
grained olivine aggregates as a function of incremental finite strains. Deformation …

Micromechanical models suggest that the onset of anelastic relaxation in polycrystalline
olivine, critical to interpretation of the seismic wave attenuation and dispersion in the upper …

We conducted experiments at high pressure (P) and temperature (T) to measure hydrogen
solubility in plagioclase (Pl) with a range of compositions (An 15 to An 94). Experiments …

We determined the kinetics of Fe‐Mg interdiffusion in ringwoodite aggregates as a function
of water content (up to~ 6,000 wt. ppm H2O) at 20 GPa and 1,373–1,673 K by the diffusion …

Fe–Mg interdiffusion rates in polycrystalline wadsleyite aggregates have been determined
as a function of water content (up to∼ 0.345 wt.% H 2 O) at 16 GPa and 1373–1773 K in a …

The detection and quantification of metal sulfides in host rocks by electrical measurements
have been priorities for field and laboratory studies, motivated by mineral prospecting and …

Olivine-hosted melt inclusions are used to investigate the hydrogen isotope compositions
(D/H) of Earth's mantle reservoirs. Studies have shown, however, that hydrogen in melt …