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Seismic velocity involves the deformation of a rock as a function of time. Compressional stress, which changes both volume and shape, leads to P-wave velocity, and shear stress, which changes shape but not volume, leads to S-wave velocity.
Seismic velocity involves the deformation of a rock as a function of time. Compressional stress, which changes both volume and shape, leads to P-wave velocity, and shear stress, which changes shape but not volume, leads to S-wave velocity.