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Bulletin of the Seismological Society of America; December 1970; v. 60; no. 6; p. 2071-2081
© 1970 Seismological Society of America
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Effects of varying anisotropy coefficient on SH-wave dispersion

S. K. UPADHYAY and JANARDAN G. NEGI

DEPARTMENT OE GEOPHYSICS BANARAS HINDU UNIVERSITY, VARANSI-5, U. P., India
THEORETICAL GEOPHYSICS DIVISION NATIONAL GEOPHYSICAL RESEARCH INSTITUTE, HYDERABAD-7, A.P. India

Abstract

The characteristic frequency equation for SH-wave propagation in an anisotropic, inhomogeneous-layered structure lying between two isotropic, homogeneous half-spaces is obtained by applying the Thomson-Haskell matrix method. A particular case is studied to analyze the effects of varying anisotropy on SH-wave dispersion. Numerical analysis is performed for a representative set of data to distinguish between the cases of increasing, uniform, and decreasing anisotropy coefficien in the medium.






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