The structure of the earth has been extensively studied using seismic waves generated by
natural earthquakes and man-made sources. In classical seismology, the earth is …

Seismic waves produced by stressed and deforming rocks lose coherence when they cross
regions of high heterogeneity. The delay in the arrival of maximum seismic energy amplitude …

The scattering of seismic waves travelling in the Earth is not only caused by random velocity
heterogeneity but also by surface topography. Both factors are known to strongly affect …

We develop a simple tomographic approach exploiting the decay rate of coda waves to map
the absorption properties of the crust in a region delimited approximately by the Rhine …

We estimated frequency-dependent attenuation of coda waves () and body waves (and) in
1.5–24 Hz by applying the single isotropic scattering theory and the extended coda …

Seismic wave attenuation in southeastern Sicily was investigated by using a data set of
about 180 local earthquakes (1.5≤ ML≤ 4.6) recorded in the period 1994–2003. We first …

The intense seismic scattering seen in Apollo lunar seismic data is one of the most
characteristic features, making the seismic signals much different from those observed on …

We investigated the high frequency attenuation of S waves in the southeastern Alps and
northern External Dinarides using waveforms from 331 earthquakes (3.0< M w< 6.5). The …

Recently, an earthquake sequence formed by a series of subsequences characterized by
large earthquakes (three events M≥ 6.0 and five events M≥ 5.0) occurred in the Central …

The relative contribution of intrinsic (Qi− 1) and scattering (Qs− 1) attenuation to seismic
wave attenuation was estimated for the Garwhal–Kumaun Himalayas using Multiple Lapse …