Using teleseimic surface-wave data from 110 selected earthquakes recorded at 10 broad-
band stations in southern Germany we construct phase-velocity maps of Rayleigh waves for …

We have determined the dispersion of fundamental mode Rayleigh waves in Southern
Germany in the frequency range 4–50 mHz by simultaneously inverting data from 66 …

We have inverted fundamental mode Rayleigh waveforms in the frequency range from 20 to
100 s to obtain a three‐dimensional S velocity distribution beneath central and southern …

Seismic surface waves exhibit much more complicated wavefields than is commonly
assumed. We are led to this conclusion after analysing 90 teleseismic events recorded at on …

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 …

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 …

Several years of broad-band teleseismic data from the GRSN stations have been analysed
for crustal structure using P-to-S converted waves at the crustal discontinuities. An inversion …

Teleseismic surface waves in general strongly deviate from plane waves as is evident from
the analysis of surface-wave data recorded with dense networks. This causes conventional …

A model of upper-mantle S-wave velocity and transverse anisotropy beneath northwestern
Europe is presented, based on regional surface wave observations. Group velocities for …

A model for the upper mantle SV-wave velocity under southern Norway is obtained by depth
inversion of the average phase velocity of the Rayleigh wave fundamental mode in the area …