论文信息 - Stress‐induced velocity anisotropy in rock: An experimental study

Stress‐induced velocity anisotropy in rock: An experimental study

Application of uniaxial stress to a sample of granite causes elastic wave velocity anisotropy. Compressional waves travel fastest in the direction of the applied stress. Two shear waves travel with generally different speeds in any direction, exhibiting acoustic double refraction which increases with increasing stress.

Gene Simmons | Amos Nur | A. Nur | G. Simmons

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