In the presence of multiple scattering, waves and particles behave fundamentally differently.
As a model for the stability of the temporal evolution of particle and wave propagation, a …

Rayleigh wave data between 20 and 120s period recorded in the western Ross Sea region
of Antarctica are inverted using the waveform inversion technique described in Passier and …

A two‐step nonlinear and linear inversion is carried out to map the lateral heterogeneity
beneath North America using surface wave data. The lateral resolution for most areas of the …

The accurate timing of seismological data is crucial for most quantitative examinations in
seismology. We present evidence that traveltime data from many stations contain systematic …

The stability of one-dimensional inverse scattering is discussed. The analysis is performed
analytically using perturbation theory for reflection coefficients that are rational functions of …

Power spectra of tomographic models of the entire earth and of models of Europe and the
Mediterranean area are compared. This comparison reveals a discrepancy (a factor 15–30) …

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 for …

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 …

Crosswell traveltime tomography is a common technique in the oil industry for determining
the velocity function in the plane between two boreholes. However, the method suffers from …

Dynamic stresses generated by earthquakes can trigger landslides. Current methods of
landslide analysis such as pseudo-static analysis and Newmark's method focus on the effects of …