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 …

This paper shows a new multidisciplinary interpretation approach to the internal structure of
Tenerife Island. The central core of this work is the determination of the three-dimensional …

Seismic waves have long been known to attenuate at a rate greater than that predicted by
geometric spreading of their wave fronts. Knopoff (1964) pointed out more than four decades …

Scattered waves observed at the seismographs of the National Italy's seismic network have
been used to investigate the intrinsic dissipation and scattering properties of the lithosphere …

It is generally accepted that the subduction polarity reversal (SPR) results from the strong
collision of two plates. Yet, the SPR of the Solomon Back‐arc Basin is started in the “soft …

The complex volcanic system of Tenerife Island is known to have a highly heterogeneous
character, as recently confirmed by velocity tomography. We present new information …

We investigated the intrinsic dissipation and scattering properties of the lithosphere under
the Friuli region (northeastern Italy) using two hypotheses:(i) a uniform earth model and (ii) …

The Canary Islands volcanic complex is studied in terms of coda wave attenuation. A
multiple lapse time window method, based on the hypothesis of multiple isotropic scattering …

Two seismic wave attenuation factors, scatteringattenuation Q s-1 and intrinsicabsorption Q i-
1 are measured using theMultiple Lapse Time Window (MLTW) analysis method forthree …

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 …