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P and S velocity structures of the Santorini–Coloumbo volcanic system (Aegean Sea, Greece) obtained by non-linear inversion of travel times and its tectonic implications

GeophysicsNon-linear InversionPlate TectonicsMarine GeologyVolcanologyEngineeringSeismologyActive TectonicsTravel TimesS Velocity StructuresRegional TectonicsGeodesyEarth ScienceTectonics