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.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Aki K (1969) Analysis of the seismic coda of local earthquakes as scattered waves. J Geophys Res 19, 74:615–631.
Aki K (1980) Attenuation of shear waves in the lithosphere for frequencies from 0.05 to5 Hz. Phys Earth Planet Int 21:50–60.
Aki K (1982) Scattering and attenuation. Bull Seismol Soc Am 72:S319–S330.
Aki K, Chouet B (1975) Origin of coda waves: source attenuation and scattering effects. J Geophys Res 80:3322–3342.
Chouet B (1976) Source scattering and attenuation effects on high frequency seismic waves. PhD Thesis, MIT Cambridge, Massachussets.
Del Pezzo E, Gresta S, Patane’ G, Patane’ D, Scarcella G (1985) Attenuation of short period seismic waves at Etna as compared to other volcanic areas. Pure Appl Geophys: 125:6.
Fehler M, Roberts P, Fairbanks T (1988) A temporal change in coda wave attenuation observed during an eruption at Mt. St. Helens. J Geophys Res 93:4367–4373.
Frankel A, Wennemberg L (1987) Energy-flux model of seismic coda: separation of Scattering and intrinsic attenuation. BSSA 77,4:1223–1251.
Gao LS, Biswas NN, Lee LC, Aki K (1983) Effects on multiple scattering on coda waves in three dimensional medium. PAGEOPH 121:3–15.
Gusev AA, Lemzikov VK (1985) Properties of scattered elastic waves in lithosphere of Kamchatka parameters and temporal variations. Tectonophysics 112:137–153.
Jin A, Aki K (1986) Temporal change in coda-Q before the Thangshan earthquake of 1976 and the Haichen earthquake of 1975. J Geophys Res 91:(B1)665–673.
Jin A, Cao T, Aki T (1895) Regional change of coda Q in the ocean lithosphere. J Geophys Res 90:8651–8659.
Kopnichev YF (1977) The role of multiple scattering in the formation of seismograms’ tail. Izv Akad Nauk SSSR Fiz Zemli 13:394–398 (English translation).
Roecker SW, Tucker B, King J, Hatzfeld D (1982) Estimates of Q in central Asia as a function of frequency and depth using the coda of locally recorded earthquakes. BSSA 72:129–149.
Rovelli A (1982) On the frequency dependence of Q in Friuli from short period digital records. BSSA 72:2369–2372.
Sato H (1977) Energy propagation including scattering effects: single isotropic scattering approximation. J Phys Earth, 25:27–41.
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1992 Springer-Verlag Berlin Heidelberg
About this paper
Cite this paper
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
Download citation
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
eBook Packages: Springer Book Archive