The role of volatile-saturation and adiabatic ascent of moderately hydrous melts on the formation of orbicules and comb layers in shallow subvolcanic conduits (Fisher Lake, Sierra Nevada).

Anders John McCarthy, University of Lausanne, Lausanne, Switzerland and Othmar Müntener, University of Lausanne, Institute of Earth Sciences, Lausanne, Switzerland
Back to: Volumes, Timescales, and Frequency of Magmatic Processes in Plutons, Chambers, and Reservoirs in the Earth's Crust II (Half Session)