AH Peslier - Journal of Volcanology and Geothermal Research, 2010 - Elsevier
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 …
EH Hauri, GA Gaetani, TH Green - Earth and Planetary Science Letters, 2006 - Elsevier
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 …
JA O'Leary, GA Gaetani, EH Hauri - Earth and Planetary Science Letters, 2010 - Elsevier
This experimental study examines the influence of tetrahedrally coordinated Al3+ (IVAl3+) on the partitioning of H+ between high-Ca clinopyroxene and silicate melt. Experiments …
The speciation and amount of water dissolved in nominally anhydrous silicates comprising eight different mantle xenoliths has been quantified using synchrotron micro-FTIR …
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 effects of dissolved H2O on the electrical conductivity and its anisotropy in olivine (Fo90) at 8GPa were investigated by complex impedance spectroscopy. At nominally …