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Coda Q in the southern Appalachians

Journal Article · · Geophysical Research Letters (American Geophysical Union); (USA)
;  [1]
  1. Virginia Polytechnic Institute and State Univ., Blacksburg (USA)
The attenuation of seismic code waves in the Southern Appalachian region was studied. Signal sources were five local and regional earthquakes and one explosion located in Ohio, Virginia and South Carolina. The data were recorded digitally by a network of seven stations in western Virginia. Joint least squares estimates of the quality factor Q, relative recording site responses and coda source amplitudes were obtained in five frequency bands using the single scattering model, and assuming body wave geometrical spreading. The results indicate a frequency dependent coda Q, represented by Q = 811 f{sup 0.42}, 1.5 {le} f {le} 12 Hz, for lapse times in the range 1.5 to 2.50 seconds. Site responses determined relative to the average network response differ by less than a factor of 2 in the range 3 to 12 Hz at five of the seven stations. However, the differences in the response of the other two sites increase with frequency, amount in to a factor of 5 at 12 Hz. Estimated relative coda source amplitude spectra exhibit similar shapes, consistent with the assumption that the scattering process is independent of path in the study region.
OSTI ID:
5668036
Journal Information:
Geophysical Research Letters (American Geophysical Union); (USA), Journal Name: Geophysical Research Letters (American Geophysical Union); (USA) Vol. 16:6; ISSN 0094-8276; ISSN GPRLA
Country of Publication:
United States
Language:
English