The minerals constituting the Earth's upper mantle are nominally anhydrous silicates
(NAMs). However they do contain hydrogen as a trace element, decorating point defects in …

Olivine, pyroxene and garnet are nominally anhydrous but can accommodate tens to
hundreds of parts per million (ppm) H2O or “water” in the form of protons incorporated in …

We present the results of an experimental study of the partitioning of water between common
upper mantle minerals (olivine, orthopyroxene, clinopyroxene, garnet) and silicate melt …

The onset of dehydration melting of nominally anhydrous peridotite can be calculated by
combination of appropriate mineral/melt partition coefficients for H2O, DHmin/liq, and a …

The water content in Earth's mantle today remains poorly constrained, but the bulk water
storage capacity in the solid mantle can be quantified based on experimental data and may …

The incorporation and diffusion of hydrogen in San Carlos olivine (Fo 90) single crystals
were studied by performing experiments under hydrothermal conditions. The experiments …

This experimental study examines the influence of tetrahedrally coordinated Al3+ (IVAl3+)
on the partitioning of H+ between high-Ca clinopyroxene and silicate melt. Experiments …

Elastic recoil detection analysis (ERDA) was used to measure the H contents of 18 synthetic
Fo90 olivines that had been hydrated to varying degrees in high pressure hydrothermal …

The speciation and amount of water dissolved in nominally anhydrous silicates comprising
eight different mantle xenoliths has been quantified using synchrotron micro-FTIR …

It has long been proposed that water incorporation in olivine has dramatic effects on the
upper mantle properties, affecting large‐scale geodynamics, and triggering high electrical …