Estimations of Q from seismic Rayleigh waves
The specific attenuation factor, Q(_γ)(^-1), has been estimated from seismic Rayleigh waves in the frequency range 0.015-0.11 Hz. The 95% confidence limits determine a narrow region around all estimates. The observational data consists of digitised Rayleigh wave traces from film chips of the long pe...
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Durham University
1973
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.450337 |