Summary
The Hindu Kush earthquake of July 6, 1962 produced anSa phase (vertical component or Rayleight type) which was clearly recorded at stations in North America in the distance range 90° to 110°. The propagation of this phase is studied in detail, both by the usual method of measuring velocity of first arrival and also by determining group velocities from the derivative of the phase of the Fourier transform (in the period range 20 to 80 seconds). The energy in theSa phase propagates in a manner intermediate between that of a single ray and that of a single isolated mode. The expected interference effects which vary as a function of distance are observed and complicate a straight-forward measurement of group velocities. The results are most reliable if only the group velocities corresponding to parts of the spectra with relatively high amplitudes are used.
The results show a regional variation in the velocity of the Rayleigh typeSa for continental areas, being higher under shield areas than under areas of more recent tectonic activity. The results are compared with theoretical calculations for the Gutenberg, Jeffreys-Bullen and Canadian Shield models of the Earth and the results indicate regional variations in shear velocity in the upper mantle extending to depths of several hundred km under continents.
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References
Don L. Anderson andM. N. Toksöz,Surface waves on a spherical earth I. Upper mantle structure from Love waves, J. Geophys. Res.68, 11 (1963), 3483.
M. Båth andA. L. Arroyo,Pa and Sa waves and the upper mantle, Geofis. Pura e Appl.56 (1963), 67.
A. Ben-Menahem,Mode Ray Duality, Bull. Seismol. Soc. Am.45 (1964), 1315.
B. A. Bolt andJ. Dorman,Phase and group velocities of Rayleigh waves in a spherical, gravitating earth, J. Geophys. Res.66, (1961), 2965.
J. N. Brune,Travel times, body waves and dispersion in the earth, Abstracts of papers submitted to the Annual Meeting of the Seismol. Soc. of Am., Seattle, Washington, Mar. 27–28 (1964).
J. N. Brune,Travel times, body waves and normal modes of the earth, Bull. Seismol. Soc. Am.54 (1964), 2099.
J. N. Brune andN. J. Dorman,Seismic weavs and earth structure in the Canadian shield, Bull. Seismol. Soc. Am.53 (1963), 167.
P. Caloi,Onde longitudinali e transversali guidate dall'astenosfera, Rendiconti dell'Accademia Nazionale dei Lincei, serie VIII, XV, fasc,6 (1953), 352.
I. Lehmann,On the travel times of P as determined from nuclear explosions, Bull. Seismol. Soc. Am.54 (1964), 123.
R. L. Kovach andD. L. Anderson,Higher mode surface waves and their bearing on the structure of the earth's mantle, Bull. Seismol. Soc. Am.54 (1964), 161.
F. Press andM. Ewing,Waves with Pn and Sn velocity at great distances, Proc. Natl. Acad. Sci. U.S.41 (1955), 24.
H. Takeuchi, M. Saito andN. Kobayashi,Theoretical dispersion curves of second mode mantle Rayleigh and Love waves for five earth models. Geophysical Notes, Geophysical Inst., Faculty of Sci., Univ. Tokyo16 (1963), 106.
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Lamont Geological Observatory, Contribution No. 883. Division of Geological Sciences, California Institute of Technology, Pasadena, Contribution No. 1378.
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Brune, J.N. TheSa phase from the Hindu Kush earthquake of July 6, 1962. PAGEOPH 62, 81–95 (1965). https://doi.org/10.1007/BF00875289
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DOI: https://doi.org/10.1007/BF00875289