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 …

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 analyse travel times of shear waves, which were recorded at the MAGNUS network, to
determine the 3D shear wave velocity (v S) structure underneath Southern Scandinavia. The …

The phase velocity dispersion of fundamental mode Rayleigh waves (period range 13-127
s) is determined by the interstation method for three profiles that traverse the North Sea …

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 …

A stacking technique is applied to measure phase velocities of the fundamental and several
higher Rayleigh modes over an array of long period stations located in Western Europe. The …

We advance evidence for the existence of seismic anisotropy in the upper mantle beneath
Southern Germany from the dispersion of Love and Rayleigh waves. The evidence is based …

We use ambient seismic noise and earthquake recordings on a temporary regional network
in southern Norway to produce Rayleigh and Love wave phase velocity maps from 3 to 67 s …

Many methods for the analysis of long-period and broad-band S-waveforms depend on a
representation of the seismic wavefield in terms of a sum of modes of a reference structure …