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Coda Q Dependence on Time, Frequency and Coda Duration Interval at Mt. Etna, Sicily

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Volcanic Seismology

Part of the book series: IAVCEI Proceedings in Volcanology ((VOLCANOLOGY,volume 3))

Abstract

A re-estimate of coda Q (Qc) was carried out on short period vertical seismograms of earthquakes located on Etna volcano, Sicily. Care was taken in selecting coda duration intervals in which the estimates are made. A clear dependence of Qc on frequency and coda duration interval has been evidenced. Qc is proportional to fn with n equal to 1 for short coda duration intervals (25 s) and with n equal to or less than 0.8 for longer codas. A depth effect and/or the presence of multiple scattering can be the cause of the Qc dependence on coda duration.

Dependence of Qc on time was investigated in an 8-year time interval.

An increase of 1/Q seems to occur before the volcanic eruptions but we cannot place a statistical significance on the results.

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© 1992 Springer-Verlag Berlin Heidelberg

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Del Pezzo, E., Patané, D. (1992). Coda Q Dependence on Time, Frequency and Coda Duration Interval at Mt. Etna, Sicily. In: Gasparini, P., Scarpa, R., Aki, K. (eds) Volcanic Seismology. IAVCEI Proceedings in Volcanology, vol 3. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-77008-1_9

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  • DOI: https://doi.org/10.1007/978-3-642-77008-1_9

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-77010-4

  • Online ISBN: 978-3-642-77008-1

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