Volatile Abundances in Basaltic Magmas and Their Degassing Paths Tracked by Melt Inclusions

Research Article| January 01, 2008 Volatile Abundances in Basaltic Magmas and Their Degassing Paths Tracked by Melt Inclusions Nicole Métrich; Nicole Métrich Laboratoire Pierre Sue CNRS-CEA, CE-Saclay Gif sur Yvette, 91191, France, nicole.metrich@cea.fr Search for other works by this author on: GSW Google Scholar Paul J. Wallace Paul J. Wallace Department 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 Author and Article Information Nicole Métrich Laboratoire Pierre Sue CNRS-CEA, CE-Saclay Gif sur Yvette, 91191, France, nicole.metrich@cea.fr Paul J. Wallace Department of Geological Sciences University of Oregon Eugene, Oregon, 97403-1272, U.S.A., pwallace@uoregon.edu Publisher: Mineralogical Society of America First Online: 13 Jul 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2008) 69 (1): 363–402. https://doi.org/10.2138/rmg.2008.69.10 Article history First Online: 13 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Nicole Métrich, Paul J. Wallace; Volatile Abundances in Basaltic Magmas and Their Degassing Paths Tracked by Melt Inclusions. Reviews in Mineralogy and Geochemistry 2008;; 69 (1): 363–402. doi: https://doi.org/10.2138/rmg.2008.69.10 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 The abundances of CO2, H2O, S and halogens dissolved in basaltic magmas are strongly variable because their solubilities and ability to be fractionated in the vapor phase depend on several parameters such as pressure, temperature, melt composition and redox state. Experimental and analytical studies show that CO2 is much less soluble in silicate melts compared to H2O (e.g., Javoy and Pineau 1991; Dixon et al. 1995). As much as 90% of the initial CO2 dissolved in basaltic melts may be already degassed at crustal depths, whereas H2O remains... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.