Earthquake Interferometer waves
An earthquake fault zone is such a scalar interferometer. Stresses and charge pileups exist in the plates on each side adjacent to the fault, with stress relief existing in the middle in the fault fracture itself. Since the rock is locally nonlinear,
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An earthquake fault zone is such a scalar interferometer. Stresses and charge pileups exist in the plates on each side adjacent to the fault, with stress relief existing in the middle in the fault fracture itself. Since the rock is locally nonlinear, the mechanical stresses and electrical currents in it are also locally nonlinear . This results in the generation of multiple frequencies of THETA 4 waves from each side of the fault interferometer, yielding two complex Fourier expansion patterns of scalar potential waves.
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An earthquake fault zone is such a scalar interferometer. Stresses and charge pileups exist in the plates on each side adjacent to the fault, with stress relief existing in the middle in the fault fracture itself. Since the rock is locally nonlinear, the mechanical stresses and electrical currents in it are also locally nonlinear . This results in the generation of multiple frequencies of THETA 4 waves from each side of the fault interferometer, yielding two complex Fourier expansion patterns of scalar potential waves.
