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Istituto Nazionale di Geofisica
Via di Vigna Murata, 605
00143 Rome, Italy
(L. M., M. D.)
Department of Earth and Atmospheric Sciences
Saint Louis University
3507 LaClede Avenue
St. Louis, Missouri 63103
(L. M., R. B. H.)
Regressions over a data set of broadband seismograms are performed to
quantify the attenuation of the ground motion in the Apennines (Italy), in the
0.255.0 Hz frequency band. The data set used in this article consists
of over 6000 horizontal-component seismograms from 446 events, with magnitude
ranging from Mw
2 to Mw = 6.0.
Waveforms were collected during recent field experiments along the Apennines.
Data from two MedNet broadband stations, located in central and southern
Apennines, were also used.
Seismograms are bandpass-filtered around a set of sampling frequencies, and
the logarithms of their peak values are written as
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A first estimate of D(r, rref, f) is
obtained using a coda normalization technique
(Aki, 1980;
Frankel et al., 1990)
and used as a starting model in the inversion of the peak values. Then, by
trial and error, the empirical D(r, rref,
f) is fitted using a trilinear geometrical spreading, with crossover
distances at 30 and 80 km, and the crustal parameter
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The final section is devoted to highlight the limitations of the formula proposed by Console et al. (1988) to estimate duration magnitudes Md in Italy.
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