Rapid evaluation of strong ground‐shaking maps after moderate‐to‐large earthquakes is
crucial to recognizing those areas where the largest damage and losses are expected …

The attenuation of coda and S waves has been inferred for the Umbria–Marche region
(central Italy) using seismic waveforms collected during the 1997 seismic crisis. The …

The attenuation of P waves, the site responses, and the source parameters (seismic
moment, corner frequency, source dimension) of 490 seismic events that occurred during …

Source and Qp parameters were estimated from the inversion of first arrival P waveform
durations of about 300 microearthquakes recorded at a digital seismic network operating in …

Many aspects of earthquake source dynamics like dynamic stress drop, rupture velocity and
directivity, etc. are currently inferred from the source time functions obtained by a …

Small magnitude earthquake data, recorded during the 1997 Umbria–Marche (Italy) seismic
crisis, have been used to study the shear wave splitting in the central Apennine. Using the …

Fault plane solutions from first motion polarity of P-waves give two nodal planes among
which it is not possible to distinguish the fault plane from the auxiliary one. We found that, for …

The study presents a detailed analysis of the swarm that occurred in the area surrounding
Sampeyre (Piedmont, Italy) during the period October–November 2010. The crisis caught …

About three-hundred microearthquakes, preceeding and accompanying the 2002-2003 Mt.
Etna flank eruption, were considered in this study. On the high-quality velocity seismograms …

A crucial point in the analysis of tectonic earthquakes occurring in a volcanic area is the
inference of the orientation of the structures along which the ruptures occur. These structures …