A note on nonequivalent quadrupole source cylindrical shear potentials which give equal displacements
Two standard integral forms of the cylindrical shear potentials for point quadrupole seismic sources, a frequency domain k-integral and a time domain Cagniardde Hoop path p-integral, are shown not to be the frequency-time domain inverse of each other. Their relationship is derived and they are shown to be seismically equivalent in that they yield the same displacement field.
Additional Information© 1978 Seismological Society of America. Manuscript received February 8, 1977. This research was supported by the Advanced Research Projects Agency of the Department of Defense and was monitored by the Air Force Office of Scientific Research under Contract F49620-77-C-0022.
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