New evidence for the serpentinization of the Palaeozoic basement of southeastern Sicily from joint 3-D seismic velocity and attenuation tomography

In this study, we derived the first 3-D P-wave seismic attenuation images (Q(P)) as well as new 3-D V-P and V-P/V-S models for the crust in southeastern Sicily. We used a large data set of local seismic events occurring in the time span 1994-2013. The results of this tomographic study have important implications on the seismic behaviour of the region. Based on velocity and attenuation images, we identified distinct volumes characterized by different fluid content, which correlate well with seismicity distribution. Moreover, the obtained velocity and attenuation tomographies help us to provide a more complete picture of the crustal structure of the area. High V-P, high Q(P) and high V-P/V-S values have been obtained in the crustal basement, below a depth of 8 km, and may be interpreted as due to the presence of Sserpentinized peridotites. Accordingly, the new model for the degree of serpentinization, retrieved from V-P values, shows that the basement has an average serpentinization value of 96 +/- 3 vol.% at 8 km, decreasing to 44 +/- 5 vol.% at about 18-20 km. Our joint interpretation of geophysical and petrophysical evidence suggests that the nature and composition of the Hyblean upper lithosphere may differ from accepted and long-established geological models, which consider this lithospheric block a continuation of the Africa continental plate.