Constraining the H2O and CO2 Contents of Basaltic Arc Magmas from Melt Inclusions: Diffusive H Loss and Shrinkage Bubble Formation, and Implications for the CO2 Contents of Primary Melts

Paul J Wallace, University of Oregon, Department of Earth Sciences, Eugene, United States, Kristina J Walowski, University of Edinburgh, School of Geosciences, Edinburgh, United Kingdom and Ellen Marie Aster, University of Oregon, Eugene, OR, United States
Back to: Fluids, Crystals, and Melts: The Role of Volatiles in Volcanic Processes from Mantle to Surface III