Probing the origins of large calderas in Kamchatka: are short-lived large silicic systems in continental arcs produced by periodic delamination of the lower crust?


Dylan Colon, University of Oregon, Earth Sciences, Eugene, OR, United States, Ilya Bindeman, University of Oregon, Department of Earth Sciences, Eugene, OR, United States and Taras Gerya, ETH Zurich, Department of Earth and Planetary Sciences, Zurich, Switzerland
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