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Simple formulae for path and amplitude anomalies of anisotropic surface waves
Author(s) -
Mochizuki E.
Publication year - 1990
Publication title -
geophysical journal international
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0956-540X
DOI - 10.1111/j.1365-246x.1990.tb00546.x
Subject(s) - great circle , amplitude , longitude , azimuth , anisotropy , surface (topology) , geology , phase (matter) , path (computing) , geodesy , surface wave , phase velocity , simple (philosophy) , geometry , geophysics , physics , latitude , optics , mathematics , philosophy , epistemology , computer science , programming language , quantum mechanics
SUMMARY Surface waves on the Earth propagate nearly on the great circle, if the anisotropy and the lateral heterogeneity are weak. Path and amplitude anomalies are approximately expressed as the intergral along the great circle. the integrand includes derivatives of the phase velocity with respect to colatitude, longitude and azimuth.

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