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Abstract: Evolution of the 2011-12 Puyehue-Cordón Caulle shallow silicic intrusion – constrained from gravity and deformation. (AGU25)

Evolution of the 2011-12 Puyehue-Cordón Caulle shallow silicic intrusion – constrained from gravity and deformation.

Diego Aron Lobos Lillo, PhD1, Francisco Delgado2, Philipp Ruprecht3, Loreto Cordova4, Christopher B Kratt5, Sara Sayyadi5, Felipe Aron6, Craig Andrew Miller7, Pablo León8, Luis Godoy8 and Matthew E Pritchard1, (1)Cornell University, Earth and Atmospheric Sciences, Ithaca, NY, United States, (2)Universidad de Chile, Department of Geology, Santiago, Chile, (3)University of Nevada Reno, Nevada Geosciences, Reno, United States, (4)Observatorio Volcanológico de los Andes del Sur (OVDAS), Servicio Nacional de Geología y Minería (SERNAGEOMIN), Temuco, Chile, (5)University of Nevada Reno, Center for Transformative Environmental Monitoring Programs (CTEMPs), Reno, United States, (6)University of Chile, Departamento de Geología, Santiago, Chile, (7)GNS Science-Institute of Geological and Nuclear Sciences Ltd, Lower Hutt, New Zealand, (8)Universidad de Chile, Santiago, Chile
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