Abstract
It is shown by the theory of elasticity that, in a non-porous medium, the velocities of compressional waves Vp and of shear waves Vs are given by the following formulae:
where E = Young’s modulus μ = shear modulus ρ = density υ = Poisson’s ratio K = modulus of elasticity All these values refer to the behaviour of a material when it is subjected to a certain stress. For example, U is a measure of the rigidity of the material.
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© 1985 Springer Science+Business Media Dordrecht
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Cordier, JP. (1985). Velocity of Seismic Waves, Relationships with the Theory of Elasticity, Variation Factors. In: Velocities in Reflection Seismology. Seismology and Exploration Geophysics, vol 3. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-3641-1_3
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DOI: https://doi.org/10.1007/978-94-017-3641-1_3
Publisher Name: Springer, Dordrecht
Print ISBN: 978-90-481-8416-3
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