Scattering and attenuation of high-frequency body waves (1-25 Hz) in the lithosphere

Details Scattering and attenuation of high-frequency body waves (1-25 Hz) in the lithosphere Scattering and attenuation of high-frequency body waves (1-25 Hz) in the lithosphere

Sep 1981

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1981pepi...26..241a&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 26, Issue 4, p. 241-243.

Physics

13

Scientific paper

A strong frequency dependence of apparent Qβ-1 of shear waves was found for the frequency range from 1 to 25 Hz using band-pass filtered records of about 900 earthquakes occurring in the central Japan area with focal depths from 0 to 150 km. The method used for estimating Qβ is a single-station method based on elimination of the source effect from S waves by the use of coda spectra. The validity of the method is confirmed by agreement between the results obtained independently using data from two stations in the same area.

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