Thermodynamics of Multi-component Gas–Melt Equilibrium in Magmas: Theory, Models, and Applications

Abstract

Research Article| May 01, 2022 Thermodynamics of Multi-component Gas–Melt Equilibrium in Magmas: Theory, Models, and Applications Paolo Papale; Paolo Papale Istituto Nazionale di Geofisica e Vulcanologia Italy Search for other works by this author on: GSW Google Scholar Roberto Moretti; Roberto Moretti Université de Paris, Institut de Physique du Globe de Paris UMR 7154 CNRS, 1 rue Jussieu F-75238 Paris FranceObservatoire Volcanologique et Sismologique de Guadeloupe Institut de Physique du Globe de Paris, Le Houelmont F-97113 Gourbeyre France Search for other works by this author on: GSW Google Scholar Antonio Paonita Antonio Paonita Istituto Nazionale di Geofisica e Vulcanologia Italy Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2022) 87 (1): 431–556. https://doi.org/10.2138/rmg.2022.87.10 Article history first online: 01 May 2022 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Paolo Papale, Roberto Moretti, Antonio Paonita; Thermodynamics of Multi-component Gas–Melt Equilibrium in Magmas: Theory, Models, and Applications. Reviews in Mineralogy and Geochemistry 2022;; 87 (1): 431–556. doi: https://doi.org/10.2138/rmg.2022.87.10 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Volatiles are the fuel and fundamental control for major processes involving magmas and volcanoes, including magma ascent, magma convection and mixing, magma differentiation, and volcanic eruptions. It is not an exaggeration to say that without volatiles in magmas the world would be a profoundly different place, and likely, life would have not flourished. Without volatiles in magmas, you would not be reading these pages. In fact, it was Earth degassing, mostly during volcanic eruptions, that provided the raw materials for the formation of the oceans and the atmosphere. Life on our planet owes much to volatiles transported with magmas and... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.