Abstract
IN 1965, Hess1 showed that seismic refraction measurements of Raitt and Shor in the East Pacific were consistent with seismic anisotropy of the uppermost mantle. Velocities between 8.0 km/s and 8.7 km/s were measured. The direction of the maximum velocity lay parallel to neighbouring fracture zones. Later, Backus2 showed that for small anisotropy the compressional wave velocity Vp(φ), measured at azimuth φ, should fit an equation of the form Coefficients J, K, L, M and N are related to elastic parameters of the upper mantle.
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References
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WHITMARSH, R. Seismic Anisotropy of the Uppermost Mantle beneath Mid-ocean Ridges. Nature 218, 558–559 (1968). https://doi.org/10.1038/218558a0
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DOI: https://doi.org/10.1038/218558a0
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