Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3551
Authors: Petrosino, S.* 
La Rocca, M.* 
Del Pezzo, E.* 
Title: Shallow velocity model of the northern flank of Stromboli Volcano, deduced by high frequency surface wave dispersion
Issue Date: 1999
Series/Report no.: 1/ 3 (1999)
URI: http://hdl.handle.net/2122/3551
Keywords: Stromboli
surface wave dispersion
Subject Classification04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology 
Abstract: The 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.
Appears in Collections:Papers Published / Papers in press

Files in This Item:
File Description SizeFormat 
08010515190508399.pdfarticle179.94 kBAdobe PDFView/Open
Show full item record

Page view(s)

91
Last Week
0
Last month
0
checked on Aug 17, 2018

Download(s)

19
checked on Aug 17, 2018

Google ScholarTM

Check