Inferring Magma Ascent Times and Reconstructing Conduit Processes in Rhyolitic Explosive Eruptions Using Reentrant H2O and CO2 Gradients


Myers Madison1, Paul J Wallace2, Colin J N Wilson3, James M Watkins2 and Yang Liu4, (1)Montana State University, Bozeman, United States, (2)University of Oregon, Department of Earth Sciences, Eugene, United States, (3)Victoria University of Wellington, School of Geography, Environment and Earth Sciences, Wellington, New Zealand, (4)Univ Tennessee, Knoxville, TN, United States
Back to: Origin and Timescales of Magmatic Systems: Discussing Ages, Rates, Transport, and Storage Processes of Magmas from the Source to Emplacement or Eruption I