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Istituto Nazionale di Geofisica
Rome, Italy
(L. M.)
Department of Earth and Atmospheric Sciences
Saint Louis University
St. Louis, Missouri
(L. M., R. B. H.)
Institute for Geosciences and Natural Resources
Hannover, Germany
(K. K.)
Regressions of 2700 horizontal-component broadband seismograms from 213
seismic events recorded by the German Regional Seismic Network (67 earthquakes
and 146 large mining explosions and rockbursts) are carried out to study the
scaling relationships of high-frequency S-wave motion for central
Europe. At a set of sampling frequencies, regressions were performed on the
logarithms of the peak amplitudes of narrow bandpass-filtered seismograms, as
well as on the logarithms of the Fourier components of the velocity spectra.
At a fixed frequency f, these values are written as
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The crustal propagation term, empirically estimated in the (0.516.0
Hz) frequency band and (40600 km) distance range, is modeled using a
complex geometrical spreading function and a frequency-dependent crustal
Q. We suggest
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A factor exp(-
0f) is used to fit the
high-frequency roll-off of the inverted excitation terms. Since we deal with
two different kinds of sources (explosions-rockbursts and earthquakes), we use
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=
30 bars, is used to fit both earthquakes and explosive excitation terms. A regression on the effective duration of the ground motion following the S-wave onset is also carried out. In central Europe, duration is observed to be almost frequency-independent. This property might be explained in terms of a self-similar distribution of crustal scatterers.
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