The primary indicators of lateral heterogeneity in the Earth are the slowness and azimuth of
incoming seismic signals. On a regional scale, surface waves in the upper mantle and crust …

Summary The stable, Precambrian East European Platform adjoins the younger, tectonically
active regions of central and western Europe along a distinct crustal boundary, the Tornquist …

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 …

Surface wave analysis was used to study possible lateral changes in the lithospheric/upper
mantle structure across the Sorgenfrei-Tornquist Zone (STZ), which is part of the transition …

We use the recently deployed ScanArray network of broad-band stations covering most of
Norway and Sweden as well as parts of Finland to analyse the propagation of Rayleigh …

This work is a part of the TOR1 project (1996–1997) and is devoted to determining the
lithospheric structure across the Sorgenfrei–Tornquist Zone in Northern Europe. For the first …

The large‐scale POLONAISE'97 seismic experiment investigated the velocity structure of the
crust and upper mantle in the Trans‐European suture zone (TESZ) region between 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 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 …

An algorithm is presented which uses the surface waveforms originating from one event
recorded in two stations which are located close to each other. The waveforms are inverted …