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- W165099533 abstract "The seismic velocity and attenuation of P, S/sub perpendicular/ and S/sub parallel/ waves traveling through a sample of Westerly Granite as it was deformed to failure under a confining pressure of 500 bars were measured. All waves were propagated in a direction normal to the axis of maximum compression, with S/sub parallel/ polarized parallel to the axis and S/sub perpendicular/ polarized normal to it. All seismic velocities had decreased from 15 to 30 percent by the time failure occurred. The amplitudes of the S/sub perpendicular/ and P waves decreased by about 30 percent. A remarkable result of the experiment is that the amplitude of the S/sub parallel/ wave increased throughout the experiment until near failure. The amplitude at 90 percent failure strength was more than twice the value under hydrostatic pressure alone. These results were explained by analyzing how modulus and dissipation due to frictional sliding at cracks are affected by the anisotropic crack distribution developed by the axial stress." @default.
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- W165099533 date "1976-12-01" @default.
- W165099533 modified "2023-09-24" @default.
- W165099533 title "Changes in velocity and attenuation of P and S waves during deformation of granite" @default.
- W165099533 hasPublicationYear "1976" @default.
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