TOMO 2 - Volcanismo y Magmatismo
MEASURING AND MODELING VOLCANIC DEFORMATION IN THE ANDES:
RESULTS AND PERSPECTIVES FROM INSAR AND GEODETIC SURVEYS.
S. Bonvalot1,2,4,6, JL. Froger1,3,5, D. Remy1,2,4, F. Bondoux1,2, G. Gabalda1,2,4, D. Legrand4, A. Pavez6, C. Robin1,3,5. (1) IRD (Institut de Recherche pour le Développement) – ([email protected], [email protected] , [email protected]) ; (2) UMR5563 Toulouse, France ; (3) UMR6524 Clermont-Ferrand, France ; (4) Facultad de Ciensas y Matematicas, Universidad de Chile ; (5) Departamento de Geología, Universidad de Chile ; (6) Institut de Physique du Globe de Paris, France.
With the aim (i) to improve our knowledge of causes and processes originating volcanic deformation in the Andes and (ii) to better monitor active volcanoes closed inhabited areas, we carried out various InSAR data acquisition in the frame of two research projects supported by the European Space Agency (ESA). New satellite ASAR-ENVISAT radar data are for instance collected for systematic surveying of the most active volcanic centers within the Andean volcanic arc, where ground deformation signals have been clearly evidenced or are highly suspected.
Figure 1 : Location of active volcanoes selected for repeated ASAR satellite surveying