Summary
Observed travel-times ofP n andS n waves are used to determine the ratio ofP n toS n velocities, Poisson’s ratio and the ratio of incompressibility to shear modulus for Europe, Japan, North America and Scandinavia. The analysis of the data reveals that theP n toS n velocity ratio decreases when theP n velocity increases for Scandinavia and North America, while the velocity ratio increases when theP n velocity increases for Europe and Japan.
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Fagernes, V., Kanestrøm, R. Variations in the upper mantle structure as derived fromP n andS n waves. PAGEOPH 109, 1762–1772 (1973). https://doi.org/10.1007/BF00876102
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DOI: https://doi.org/10.1007/BF00876102