To advance our understanding of the complex and episodic tectonic history of the central
Mediterranean, we image the characteristics and structure of the convergent African and …

The inverse tomography method has been used to study the P-and S-waves velocity
structure of the crust and upper mantle underneath Iran. The method, based on the principle …

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 …

We present a new model of P-velocity anomalies in the upper mantle beneath the Arabian
Peninsula, Red Sea, and surrounding regions. This model was computed with the use of …

We present the first results of a high-resolution teleseismic traveltime tomography and
seismic anisotropy study of the lithosphere–asthenosphere system beneath the western …

The Quaternary Eifel volcanic fields, situated on the Rhenish Massif in Germany, are the
focus of a major interdisciplinary project. The aim is a detailed study of the crustal and …

We construct a new three‐dimensional S velocity model and Moho map by jointly inverting
regional S and Rayleigh waveform fits, teleseismic S and SKS arrival times, fundamental …

We analyze data from the French Laboratoire de Detection Geophysique (LDG) network of
digital short-period seismic stations. The P-waves from several earthquakes in the Kuril …

We use International Seismological Centre (ISC) P arrival data (1964–1987) and iterative
algorithms which minimize the l1 and l2 residual norms to solve simultaneously for three …

Despite immense progress in imaging seismic velocity anomalies in the mantle over the past
15 years, we still know relatively little about their physical cause. One way to shed some light …