The upper mantle velocity structure beneath Europe is investigated by body-wave modelling
of broad-band seismograms from earthquakes in the eastern Mediterranean recorded by …

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 …

The crustal structure has been determined in the area between the Lorraine, the Bohemian
massif and the northern Alps with considerable detail in recent years. But up to now little has …

Over the past 20 years the study of P-and S-wave velocities in the upper mantle of the
European-Mediterranean area has been the subject of intensive research work. We present …

A set of two hundred shear-wave velocity models of the crust and uppermost mantle in
southeast Europe is determined by application of a sequence of methods for surface-waves …

P waveforms of regional crustal earthquakes have been modeled to obtain an upper mantle
compressional velocity model for the West Mediterranean Basin. Data come from long …

In a particular region a smoothed and averaged representation of the velocity structure in the
upper mantle can be derived from long-period body wave and higher-mode surface wave …

An inversion of ISC travel-time data from selected earthquakes in the distance range 30°–
90° to 53 stations in Central Europe has been used to model velocity down to 600 km depth …

We have detected what appear to be strong lateral variations in upper mantle shear-wave
velocities under Europe and western Eurasia. The evidence suggests that the Alpine belt of …

A large-scale three-dimensional inversion of teleseismic P wave arrival times from ISC
bulletins is performed over the part of Europe extending from Scandinavia to the Alps, and …