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- W2124583151 abstract "Asymptotic results are derived for the travel times and amplitudes of waves diffracted by surfaces of discontinuity in the Earth's mantle. A canonical problem, defined to be that of diffraction by a uniform elastic or visco-elastic sphere in a uniform elastic medium, is first solved asymptotically and the result applied, by means of simple ray theory, to an Earth model which is spherically symmetric except for the diffracting discontinuity. Some calculations are carried out for comparison with the signals from the Bukhara explosion discussed by Douglas et al. and an attempt is made to identify their arrival PH1 with a diffracted arrival from a mantle discontinuity. To explain the low amplitude of the direct wave a dissipative region in the mantle, which is avoided by the diffracted wave, is postulated and the approximate values of Q needed to equate the amplitudes of direct and diffracted waves are calculated." @default.
- W2124583151 created "2016-06-24" @default.
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- W2124583151 date "1973-05-01" @default.
- W2124583151 modified "2023-09-23" @default.
- W2124583151 title "Diffraction by Anomalous Regions in the Earth's Mantle" @default.
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- W2124583151 doi "https://doi.org/10.1111/j.1365-246x.1973.tb05833.x" @default.
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