Two-dimensional seismic attenuation images of Stromboli Island using active data

In this work we present intrinsic and scattering seismic attenuation 2-D images of Stromboli
Volcano. We used 21,953 waveforms from air gun shots fired by an oceanographic vessel and recorded
at 33 inland and 10 ocean bottom seismometer seismic stations. Coda wave envelopes of the filtered
seismic traces were fitted to the energy transport equation in the diffusion approximation, obtaining a
couple of separate Qi and Qs in six frequency bands. Using numerically estimated sensitivity kernels for
coda waves, separate images of each quality factor were produced. Results appear stable and robust. They
show that scattering attenuation prevails over intrinsic attenuation. The scattering pattern shows a strong
concordance with the tectonic lineaments in the area, while an area of high total attenuation coincides with
the zone where most of the volcanic activity occurs. Our results provide evidence that the most important
attenuation effects in volcanic areas are associated with the presence of geological heterogeneities.