The Sulfur Budget in Magmas: Evidence from Melt Inclusions, Submarine Glasses, and Volcanic Gas Emissions

Abstract

Research Article| January 01, 2011 The Sulfur Budget in Magmas: Evidence from Melt Inclusions, Submarine Glasses, and Volcanic Gas Emissions Paul J. Wallace; Paul J. Wallace Deprtment of Geological Sciences, University of Oregon Eugene, Oregon 97403-1272, U.S.A., pwallace@uoregon.edu Search for other works by this author on: GSW Google Scholar Marie Edmonds Marie Edmonds Department of Earth Sciences University of Cambridge Cambridge, CB2 3EQ, United Kingdom, medm06@esc.cam.ac.uk Search for other works by this author on: GSW Google Scholar Author and Article Information Paul J. Wallace Deprtment of Geological Sciences, University of Oregon Eugene, Oregon 97403-1272, U.S.A., pwallace@uoregon.edu Marie Edmonds Department of Earth Sciences University of Cambridge Cambridge, CB2 3EQ, United Kingdom, medm06@esc.cam.ac.uk Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2011) 73 (1): 215–246. https://doi.org/10.2138/rmg.2011.73.8 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Paul J. Wallace, Marie Edmonds; The Sulfur Budget in Magmas: Evidence from Melt Inclusions, Submarine Glasses, and Volcanic Gas Emissions. Reviews in Mineralogy and Geochemistry 2011;; 73 (1): 215–246. doi: https://doi.org/10.2138/rmg.2011.73.8 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 The major magmatic volatile components—H2O, CO2, S, Cl, and F— play an important role in the formation, evolution, and eruption of magma. Knowledge of magmatic concentrations and fluxes of these volatiles is thus important for understanding explosive eruptive behavior of volcanoes, recycling of volatiles in subduction zones, formation of magmatic-hydrothermal ore deposits, fluxes of volcanic gases to Earth’s atmosphere, and potential climatic impacts of large volcanic eruptions. Over the past 30 years, new analytical techniques for measuring volatiles in melt inclusions and glasses from volcanic rocks and new developments in remote sensing technology used for quantifying... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.