Along Strike Variation in Eruptive and Decompression Rates for Rhyolite-Obsidian Domes, South Sister Volcano, OR


Laura E Waters, Sonoma State University, Geology, Rohnert Park, CA, United States and Benjamin James Andrews, National Museum of Natural History, Smithsonian Institution, Mineral Sciences, Washington, 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