Abstract
abstract The attenuation of longitudinal body waves generated by local shocks in southern Peru was investigated. Thirty-four shocks, with focal depths between 20 and 180 km, were used in the study of attenuation as a function of depth and as a function of frequency (1-30 cps). Shocks were recorded on magnetic tape at three stations along the western flank of the Andes. The dimensionless specific attenuation factor Q was computed from measurements of the relative change in shape of P-particle velocity spectra with distance from the source. Near surface effects on amplitudes were taken into account. It was found that: Qp(1.5-15 cps) > 1 × 103; the attenuation of P waves increases markedly above 15 cps, probably due to scattering losses; and although absolute Qp values as a function of depth could not be resolved, an increase in P wave attenuation at a depth of about 80 km is suggested. Vp/Vs, determined from S-P and P readings at seven stations for 150 shocks, is significantly higher for oceanic shocks than inland shocks.
References
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Dates
Type | When |
---|---|
Created | 4 years, 1 month ago (July 14, 2021, 12:34 p.m.) |
Deposited | 4 years, 1 month ago (July 14, 2021, 12:35 p.m.) |
Indexed | 1 year, 1 month ago (July 26, 2024, 3:54 a.m.) |
Issued | 58 years, 5 months ago (April 1, 1967) |
Published | 58 years, 5 months ago (April 1, 1967) |
Published Online | 58 years, 5 months ago (April 1, 1967) |
Published Print | 58 years, 5 months ago (April 1, 1967) |
@article{Sumner_1967, title={Attenuation of earthquake generated P waves along the western flank of the Andes}, volume={57}, ISSN={0037-1106}, url={http://dx.doi.org/10.1785/bssa0570020173}, DOI={10.1785/bssa0570020173}, number={2}, journal={Bulletin of the Seismological Society of America}, publisher={Seismological Society of America (SSA)}, author={Sumner, Roger D.}, year={1967}, month=apr, pages={173–190} }