Roberto Moretti

TL;DR: Papale et al. as mentioned in this paper applied thermodynamic equilibrium between gaseous and liquid volatile components to model the volatile saturation surface in H 2 O−CO 2 -silicate melt systems.

TL;DR: In this article, the results of two years of real-time observation of H2O, CO2, and SO2 in volcanic gases from Mount Etna volcano were unambiguously demonstrated that increasing CO2/SO2 ratios can allow detection of pre-eruptive degassing of rising magmas.

TL;DR: In this article, the authors present LA-ICP-MS data for garnets from the Crown Jewel Au-skarn deposit (USA), and discuss the factors controlling incorporation of REE into garnets, and strengthen the potential of garnet REE geochemistry as a tool to help understand the evolution of metasomatic fluids.

TL;DR: The analysis of gaseous compositions from Solfatara (Campi Flegrei, South Italy) fumaroles since the early 1980s, clearly reveals a double thermobarometric signature.

TL;DR: The first studies on sulfur isotope geochemistry were performed approximately sixty years ago (e.g., Thode et al. 1949; Trofimov 1949) and have been used to highlight and investigate several processes, such as the evolution of the solar system; the oxidation of the Earth's atmosphere and hydrosphere; the genesis of ore deposits and fossil fuels (coal, oil, and gases); the origin and provenance of S species in different natural fluids, including groundwater, rainwater, as well as present-day and ancient marine waters (as recorded by evaporite