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  • 1
    Publication Date: 2017-04-04
    Description: The Local-Magnitude scale actually in use at Vesuvius Observatory is based on the measure of seismogram coda duration, and calibrated with data from Irpinia aftershocks. A recent study on local seismic attenuation at Mt. Vesuvius reveals coda shapes highly different from those from Irpinia aftershocks, and a very low quality factor, if compared to the average Q of the region, indicating the necessity of the revision of the Magnitude scale, in order to better compare the seismic energy associated to the local seismicity of Mt. Vesuvius to that of other active volcanoes. Being the seismic attenuation parameters known in the area, we could correct the seismic amplitudes for the path effect to obtain precise estimates of the amplitude level of the displacement spectrum. Hence we estimated the Moment-Magnitude, MW, for a set of well recorded micro-earthquakes. To use the Richter formula ML = log10Amax −log A0(R) we estimated the log Amplitude-Distance correction curve, −logA0(R), numerically synthesizing an S-wave-packet and letting it propagate in a earth medium with the same attenuation properties of those measured at Mt. Vesuvius. Then we synthesized the Wood-Anderson equivalent seismogram for the same data set and used the distance correction in order to calculate the Wood-Anderson Magnitude. This Magnitude scale was normalized in order to fit the Richter formula valid for Southern California at a distance 1 of 10 km, and results to be MWA = log A+ 1.34log(R)−1.10. The comparison of the Wood-Anderson scale with the Duration- Magnitude scale in routine use at Vesuvius Observatory indicates that care must be taken when the estimate of the Duration-Magnitude is carried out for small earthquakes recorded at a site characterized by a high level of seismic noise.
    Description: Published
    Description: 207-215
    Description: JCR Journal
    Description: reserved
    Keywords: Local magnitude ; volcano seismicity ; 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2017-04-04
    Description: 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.
    Description: Published
    Description: 83-94
    Description: JCR Journal
    Description: reserved
    Keywords: Stromboli ; surface wave dispersion ; 04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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