Amplitudes of Fundamental Seismic Waves in the Mantle

  • L. M. Kilinchuk
  • T. B. Yanovskaya


The interpretation of seismological observations at all distances, except the very nearest (out to 10°), is based on the basic compendium of seismic-wave travel times composed by Jeffreys and Bullen in 1940 [1] and later refined and supplemented by a number of authors [10].


Seismic Wave Focal Depth Body Wave Source Depth Seismic Wave Prop 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


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Literature Cited

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    Jeffreys, H., and K. E. Bullen (1940), Seismological Tables, London, British Association for the Advancement of Science, Gray-Milne Trust.Google Scholar
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    Bullen, K. E. (1938), “Theoretical travel times of the phases PP, PPP, PS, PPS, SS, PSS, and SSS,” in: Mon. Not. Roy. Astr. Soc., Geophys. Suppl., 4:583–593.Google Scholar
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    Anderson, D. L., A. Ben-Menahem, and C. B. Archambeau (1965), “Attenuation of seismic energy in the upper mantle,” J. Geophys. Res., 70:1441–1448.CrossRefGoogle Scholar
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    Kilinchuk, L. M., and T. B. Yanovskaya (1966), “The amplitude ratio PP/P,” in: Computational Seismology, No. 2, pp. 71–82, Moscow, Nauka.Google Scholar

Copyright information

© Consultants Bureau, New York 1972

Authors and Affiliations

  • L. M. Kilinchuk
  • T. B. Yanovskaya

There are no affiliations available

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