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On one side, over the T element (Love waves) the existence of a thin shallow stiff level excites greater settings whose top velocity is managed because of the shear-wave velocity for the deeper layers. On the other side, such a stiff level doesn't massively affect the velocity spectra of the Z and R components (Rayleigh waves) in addition to relevant RPM irrespective regarding the presence of this shallow rigid level, RPM obviously shows the alteration from retrograde to prograde as a result o