Modeling of the EM inductive‐limit surface currents

Author:

King Andrew1,MacNae James C.1

Affiliation:

1. Co‐operative Research Center for Australian Mineral Exploration Technologies, School of Earth Sciences, Macquarie University, N. Ryde, New South Wales 2109, Australia. Emails:

Abstract

The inductive limit of an electromagnetic (EM) response, which is the early time or infinite‐frequency response, may be quickly and efficiently calculated when compared to the effort and time required to calculate a full 3-D EM model. This can be achieved through matrix solution of a simple set of simultaneous conditions that any primary magnetic field must not penetrate the target body. In airborne EM (AEM) data acquisition, hundreds of local anomalies may need to be interpreted each day of flying, and the inductive limit modeling algorithm provides a useful and very fast model for realistic target geometries. In particular, it allows typical single‐peaked field anomalies in the vertical component of fixed‐wing AEM systems to be fitted, using a multi‐faceted solid body. Thin‐plate models, which are commonly used, produce “M-shaped” responses rarely seen in field data.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference16 articles.

1. Asten, M., 1999, Modeling in mining geophysics; in Oristaglio, M., and Spies, B., Eds., Three‐dimensional electromagnetics: Soc. Expl. Geophys., 477–488.

2. Bailey, R. C., and Cheeseman, S., 1996, A multigrid solver for inductive limit EM responses in orebody delineation: 66th Ann. Internat. Mtg., Soc. Expl. Geophys., Expanded Abstracts, 265–268.

3. Grant, F. S., and West, G. F., 1965, Interpretation theory in applied geophysics: McGraw‐Hill.

4. Griffiths, D. J., 1981, Introduction to electrodynamics: Prentice‐Hall.

5. Harrington, R. F., 1968, Field computation by moment methods: Macmillan Publ. Co.

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