Gas–Solid Reactions in Arc Volcanoes: Ancient and Modern

Abstract

Research Article| November 01, 2018 Gas–Solid Reactions in Arc Volcanoes: Ancient and Modern Richard W. Henley; Richard W. Henley Department of Applied Mathematics Research School of Physics and Engineering The Australian National University ACT Australia Search for other works by this author on: GSW Google Scholar Terry M. Seward Terry M. Seward School of Geography, Environment and Earth Sciences Victoria University Wellington New Zealand Search for other works by this author on: GSW Google Scholar Author and Article Information Richard W. Henley Department of Applied Mathematics Research School of Physics and Engineering The Australian National University ACT Australia Terry M. Seward School of Geography, Environment and Earth Sciences Victoria University Wellington New Zealand Publisher: Mineralogical Society of America First Online: 09 Nov 2018 Copyright © 2018 by the Mineralogical Society of AmericaMineralogical Society of America Reviews in Mineralogy and Geochemistry (2018) 84 (1): 309–349. https://doi.org/10.2138/rmg.2018.84.9 Article history First Online: 09 Nov 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Richard W. Henley, Terry M. Seward; Gas–Solid Reactions in Arc Volcanoes: Ancient and Modern. Reviews in Mineralogy and Geochemistry 2018;; 84 (1): 309–349. doi: https://doi.org/10.2138/rmg.2018.84.9 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 Arc volcanoes are most commonly defined in terms of their magmatic and eruptive histories but the sustained flux of high temperature reactive gases through them, at all stages of their eruptive cycles, equally defines them as large scale, gas phase, chemical reactors (Fig. 1). Inside them, reactive mass transfer occurs continuously as magmatic vapor, released from crystallizing silicate melt at lithostatic pressure, expands through a subsurface volcanic gas plume (Henley and McNabb 1978) to atmospheric pressure at the surface. Between eruptions, volcanic gas fluxes dominated by water and reactive gases, such as SO2(g) and HCl... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.