We present a new tomographic model for P-and S-velocity anomalies beneath Europe (30°
N–55° N, 5° W–40° E), extending in depth up to 700 km and constrained by inversion of data …

A model of seismic P and S anomalies in the upper mantle beneath Asia (in limits of 35° E–
140° E, 12° N–57° N) was constructed based on the tomographic inversion of traveltime …

This paper presents a 3-D regionalized model of the European crust and mantle velocity
structure down to depths of approximately 300 km. The model is entirely based upon the …

Summary A new model, EUR-S91, of shear-wave velocity variations in the upper mantle
beneath central Europe and surrounding regions, down to a depth of 670km, is presented …

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 …

The 3-D P-wave velocity structure of the mantle below Europe, the Mediterranean region
and a part of Asia Minor is investigated. This study is a considerable extension of an earlier …

Temperature is one of the key parameters controlling lithospheric and mantle dynamics and
rheology. Using recent experimental data on elastic parameters and anelasticity, we obtain …

Subducted slab roll-back, lithospheric instability and asthenospheric extrusion have all been
proposed as mechanisms that explain the evolution of the extensional Pannonian Basin …

The P-wave velocity structure of the mantle below the Iberian Peninsula is investigated with
the method of delay-time tomography. More than 200,000 delay-times are inverted for …

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 …