3-D Q-coda attenuation structure at Mt. Etna (Italy)

Abstract

Summary Three dimensional attenuation images of Mt. Etna volcano obtained by the analysis of Q-coda from local volcano-tectonic earthquakes are presented in this work. Seismic sources are confined inside the Etna structure with a maximum focal depth of 35 km below the sea level. The space distribution of the attenuation values was calculated by using 3-D weighting functions derived by the sensitivity kernels of Pacheco and Snieders (2006) and approximated by a polynomial interpolation, represented in the maps by using a back- projection method. Data were analyzed in four bands with central frequency placed at 1.5, 3, 6 and 12 Hz respectively. We observed a frequency dependence of Q-coda with values that range from 55 at 1.5 Hz to 218 at 12 Hz. Q-coda space distribution in the Etna area shows almost uniformity in the average attenuation in the first 35 km below the surface. The images were derived with a resolution of 5 km. We observe as one of our main conclusions that Q-coda attenuation space anomalies are correlated with the areas of highest structural heterogeneities and are distributed along the well-known tectonic structures which characterize the crust in Mt. Etna region. Previous and numerous velocity and attenuation images describing the structure of Mt. Etna support our main conclusion: high Q-coda volumes almost coincide with the zones marked by high velocity and relative low total attenuation for direct waves.