Interpreting H2O and CO2 Contents in Melt Inclusions: Constraints from Solubility Experiments and Modeling

Abstract

Research Article| January 01, 2008 Interpreting H2O and CO2 Contents in Melt Inclusions: Constraints from Solubility Experiments and Modeling Gordon Moore Gordon Moore Department of Chemistry & Biochemistry, Arizona State University Tempe, Arizona, 85287-1604, U.S.A., gordon.moore@asu.edu Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2008) 69 (1): 333–362. https://doi.org/10.2138/rmg.2008.69.9 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 Gordon Moore; Interpreting H2O and CO2 Contents in Melt Inclusions: Constraints from Solubility Experiments and Modeling. Reviews in Mineralogy and Geochemistry 2008;; 69 (1): 333–362. doi: https://doi.org/10.2138/rmg.2008.69.9 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 Due to their volatile nature and low solubility in silicate melts at the surface of the Earth, the direct measurement of the volatile components H2O and CO2 in magmatic systems is dependent on the presence of glass inclusions trapped in a crystal host prior to eruption. These inclusions, along with the glassy rinds of submarine pillow lavas, represent one of the few windows researchers have into the pre-eruptive chemical characteristics of magmatic systems (e.g., Anderson et al. 2000; Roggensack 2001a; Metrich and Wallace 2008). This information is critically important, as it is volatile exsolution... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.