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Mathematical Modeling of G type Seismic Waves in a Homogeneous Layer over a Transversely Isotropic Half-space under Initial Stress

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Figure

Fig. 1.Geometry of the problem
Fig. 4 and Fig. 5. In Fig. 4 shows the variation in  /
Fig 7: Variation of group velocity  Uparameter   with respect to k  and s  for different stress parameters

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