▪ Abstract The Re-Os isotope sytem, based on the long-lived β− transition of 187Re to
187Os, has matured to wide use in cosmochemistry and high-temperature geochemistry …

Arc-basaltic melts of typical hydration state (≥ 2 wt% H 2 O) are buoyant relative to all
common crustal igneous rock types and may pass adiabatically from a mantle source …

Magmatic-hydrothermal ore deposits in collisional orogens are new targets for modern
mineral exploration, yet it is unclear why they preferentially occur in some specific tectonic …

Owing to advances in microanalytical techniques over the last 15 years, there is a growing
database on the volatile contents of subduction-related magmas as recorded in melt (glass) …

Silicate Glasses and Melts, Second Edition describes the structure-property-composition
relationships for silicate glasses and melts from a geological and industrial perspective …

The sulfur contents at sulfide saturation (SCSS) of a basaltic and a picritic melt have been
measured experimentally as a function of pressure and temperature from 5 to 90 kb and …

The analysis of volatiles in magmatic systems can be used to constrain the volatile content of
the Earth's mantle and the influence that magmatic degassing has on the chemistry of the …

XANES analyses at the sulfur K-edge were used to determine the oxidation state of S
species in natural and synthetic basaltic glasses and to constrain the fO2 conditions for the …

The composition of gases released from volcanoes is a function of deep processes, such as
vapor-melt separation during the generation and rise of the magmas, and shallow …

Water and carbon dioxide comprise the most abundant volatile species in most magmas, yet
other volatile species are also of interest for a wide variety of reasons, ranging from their …