Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3551
AuthorsPetrosino, S.* 
La Rocca, M.* 
Del Pezzo, E.* 
TitleShallow velocity model of the northern flank of Stromboli Volcano, deduced by high frequency surface wave dispersion
Issue Date1999
Series/Report no.1/ 3 (1999)
URIhttp://hdl.handle.net/2122/3551
KeywordsStromboli
surface wave dispersion
Subject Classification04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology 
AbstractThe wavefield produced by the Stromboli volcano explosion quakes shows a significant amount of surface waves. Rayleigh waves recorded by a linear array have been investigated to infer the shear-wave velocity model of the Stromboli northern flank. The group velocity dispersion curve was obtained using the multiple filter technique, while the phase velocity dispersion curve was calculated both by phase-matched filtering and performing a p–omega stack on the observed waveforms. Through the inversion of these curves we were able to recover the shear-wave structure to a depth of about 190 m.
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