Decadal to monthly timescales of magma transfer and reservoir growth at a caldera volcano

T. H. Druitt (), F. Costa, E. Deloule, M. Dungan and B. Scaillet
Additional contact information
T. H. Druitt: Clermont Université, Université Blaise Pascal, Laboratoire Magmas et Volcans, BP 10448, F-63000 Clermont-Ferrand, France
F. Costa: Earth Observatory of Singapore, Nanyang Technological University, Singapore 639798
E. Deloule: CRPG-CNRS, BP20, 54501 Vandoeuvre les Nancy, France
M. Dungan: Université de Genève, Rue des Maraîchers, 13 CH-1205 Genève, Switzerland
B. Scaillet: ISTO–UMR 6113 CNRS/Université d'Orléans/Université Francois Rabelais de Tours, 1A rue de la Ferollerie, 45071 Orleans, France

Nature, 2012, vol. 482, issue 7383, 77-80

Abstract: A study of pre-eruptive magmatic processes at a caldera volcano shows that, although such a volcano may have been dormant for a long period, its magma reserves may be replenished in a comparatively very short time and it may move rapidly from a quiescent state to one on the verge of eruption.

Date: 2012
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DOI: 10.1038/nature10706

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