The angular frequency associated with them at the cutoff for the nth higher mode is given by the product of the mode number and π over H times 1 over the square root of the difference in the inverse squares of velocity constants β1 and β2 during propagation.
The angular frequency associated with them at the cutoff for the nth higher mode is given by the product of the mode number and π over H times 1 over the square root of the difference in the inverse squares of velocity constants β1 and β2 during propagation. Their particle motion is toroidal and always perpen-dicular to the propagation vector, and may be found on the transverse record of a seismogram. For ten points, name these dispersive surface waves that form from constructive interference of S-wave reflections between trapping layers, which arrive at a seismograph just prior to Rayleigh Waves.
The angular frequency associated with them at the cutoff for the nth higher mode is given by the product of the mode number and π over H times 1 over the square root of the difference in the inverse squares of velocity constants β1 and β2 during propagation.
Love waves