Attenuation of body waves in Southeastern Sicily (Italy)

Physics

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Scientific paper

The attenuation of P- and S-waves in Southeastern Sicily was estimated by applying two different methods in time and frequency domains. We analyzed waveforms from about 290 local events (0.6<=ML<=4.6) recorded at a three-component digital network.
By applying the pulse broadening method to the first P-wave pulse, we found an average Qp value of ca. 140. The application of the frequency decay method provided a Qp value of ca. 120, in the low-frequency band (3-9Hz). Conversely, in the high frequency range (16-27Hz) the average Qp is significantly larger (ca. 640). The frequency decay method was also applied to S-waves spectra. In the low frequency range (2-5Hz) the estimated average Qs is ca. 190. As for Qp, also Qs, in the high frequency range (16-27Hz), is larger (ca. 700). These results evidenced a frequency dependence of both the quality factors Qp and Qs, as commonly observed in tectonically active zones characterized by high degree of heterogeneity.

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