In this paper we present P wave tomographic images of the mantle beneath Italy obtained by
inverting∼ 6000 teleseismic P and PKP wave arrival times, accurately repicked, recorded in …

We study the upper mantle P wave velocity structure below the Euro‐Mediterranean area,
down to 1000 km depth, by seismic travel time tomography. We invert summary residuals …

In this paper we present a 3-D image of the P-wave velocity structure in the crust and
uppermost mantle beneath Italy, obtained by inverting P-wave arrival times of crustal …

This paper presents a velocity model of the Italian (central Mediterranean) lithosphere in
unprecedented detail. The model is derived by inverting a set of 166,000 Pg and Pn seismic …

Recent tomographic investigations performed down to~ 300 km depth in the Calabrian Arc
region gave insight in favor of the hypothesis that the Ionian subducting slab is continuous in …

The velocity-depth distribution of the lithosphereasthenosphere in the Italian region and
surroundings is imaged, with a lateral resolution of about 100 km, by surface wave velocity …

27,646 P-and 15,025 S-wave readings obtained from 2238 earthquakes and 84 artificial
sources were used to perform tomographic inversion of P velocity and VP/VS ratio in the …

Teleseismic waveforms recorded by a regional array crossing the northern Italian peninsula
and northern Corsica are analyzed using the receiver function technique, to determine the …

Travel times of P-waves in the Euro-Mediterranean region show strong and consistent
lateral variations, which can be associated to structural heterogeneity in the underlying crust …

The 3-DP-wave velocity structure of the Alpine crust has been determined from local
earthquake tomography using a set of high-quality traveltime data. The application of an …