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Published October 1964 | Published
Journal Article Open

Spectral response of an elastic sphere to dipolar point-sources

Abstract

A stratified elastic sphere is excited by an harmonic dipolar source of arbitrary orientation and depth. The total field is expanded in series of vector spherical harmonics and then condensed into a convenient form of a displacement dyadic. The Haskell-Gilbert matrix method is employed to obtain the radial factor of the displacements for a multilayered sphere. The dependence of the field on the azimuth angle and the fault elements is obtained for the case of a double-couple at depth. Expressions are also developed for the radiation pattern of surface waves over a spherical stratified earth.

Additional Information

Copyright © 1964, by the Seismological Society of America. Manuscript received May 22, 1964. This research was supported by Contract No. AF-49(638)-1337 of the Air Force Office of Scientific Research as part of the Advanced Research Projects Agency project VELA.

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Created:
August 19, 2023
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October 17, 2023