Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8409
AuthorsBruno, V.* 
Mattia, M.* 
Aloisi, M.* 
Palano, M.* 
Cannavò, F.* 
Holt, W. E.* 
TitleGround deformations and volcanic processes as imaged by CGPS data at Mt. Etna (Italy) between 2003 and 2008
Issue Date21-Jul-2012
Series/Report no./117 (2012)
DOI10.1029/2011JB009114
URIhttp://hdl.handle.net/2122/8409
KeywordsMt. Etna ground deformations
Volcano monitoring
Strain rate analysis
Volcanic source modelling
Subject Classification04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations 
04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring 
AbstractWe analyze the kinematic and crustal deformations of Mt. Etna from 2003 to 2008 as imaged by the Mt. Etna continuous GPS (CGPS) network (Etna@net). Through a careful analysis of GPS time series, six coherent phases of crustal deformations have been identified, three inflation phases and three deflation phases, superimposed on a major inflation of the volcanic edifice since 2001. The inversions of GPS velocities have enabled: 1) a better understanding of the evolution of the volcanic sources acting beneath the volcano; 2) analysis of the strain rate patterns; and 3) a delineation of potential coupling between volcanic sources and the observed ground deformations. The modelling of the pressure sources has shown a separation between inflation and deflation sources. The deflation sources show an upward migration, from 5.5 toward 2.0 km (b.s.l.), while the inflation sources are located within 5.5 and 4.0 km (b.s.l.). Our results indicate that the kinematic and ground deformations of the mid-upper eastern flank are driven by the interplay between the effect of the magmatic sources and a south-eastward motion. Furthermore, clockwise rotations have been detected that prevailed over the eastern motion of the flank during the inflation phase preceding the 2004-2005 and 2006 eruptions. Finally, the accordance between the higher geodetic shear strain rates and the area with the highest seismic energy release shows that measured geodetic shear strain rates can provide useful information on the potential occurrence of seismic activity.
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