EM Response of an Arbitrary Source on a Layered Earth, A New Computational Approach
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1972-11
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Abstract
The Fast Fourier transform is used to compute the EM Induction response in a layered earth by an arbitrary grounded or ungrounded source (e.g. dipole, Turam looo, grounded wire). The induction problem is expressed in the horizontal wavenumber domain, the 2-D Fourier transform of the x-y plane, where a source term and an earth transfer function may be considered separately. This new procedure results in a significant reduction in computation time and flexible straightforward programming. Several examples are described to demonstrate the advantages and limitations of the method.
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This paper was presented at the 42nd Annual Meeting of the Society of Exploration Geophysicists in Anaheim, California on November 28, 1972. (Mining Session, paper M-12). This paper appeared in Research in Applied Geophysics, No. 5, Geophysics Laboratory, University of Toronto, Canada.
Keywords
Geophysics, Research in Applied Geophysics
Citation
Lajoie, J., Alfonso-Roche, J. and G.F. West. (1972) EM Response of an Arbitrary Source on a Layered Earth, A New Computational Approach. Research in Applied Geophysics, No. 5, Geophysics Laboratory, University of Toronto, Canada.
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