Regionalization and dependence of coda Q on frequency and lapse time in the seismically active Peloritani region (northeastern Sicily, Italy)
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/article/10.1007/s10950-018-9750-0/fulltext.html
Reference101 articles.
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2. Aki K (1980) Attenuation of shear-waves in the lithosphere for frequencies from 0.05 to 25 Hz. Phys Earth Planet Inter 21:50–60
3. Aki K, Chouet BA (1975) Origin of coda waves: source, attenuation and scattering effects. J Geophys Res 80:3322–3342
4. Akinci A, Taktak G, Ergintav S (1994) Attenuation of coda waves in the western Anatolia. Phys Earth Planet Inter 87:155–166
5. Azzaro R, Bernardini F, Camassi R, Castelli V (2007) The 1780 seismic sequence in NE Sicily (Italy): shifting an underestimated and mislocated earthquake to a seismically low rate zone. Nat Hazards 42:149–167. https://doi.org/10.1007/s11069-006-9066-1
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