Abstract
Various workers have appealed to Biot-Savart's law for interpreting their anomalous geomagnetic response functions as an aid to describing the electromagnetic induction process. This approach, of using such a line current analogue, is shown herein to be erroneous if the conductivity of the lower half-space is not taken into consideration. A numerical solution, using an FFT, is derived from the kernels of the electromagnetic field components involved, and is compared with the simplistic solution offered by Biot-Savart's static field approximation. Uses of a line current in a conducting half-space as a suitable analogue of the true induction processes are illustrated with comparison to 3 anomalies - a conducting block, Alert, and the Great Glen fault.-Author
Original language | English |
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Pages (from-to) | 56-62 |
Number of pages | 7 |
Journal | Journal of Geophysics - Zeitschrift fur Geophysik |
Volume | 60 |
Issue number | 1 |
Publication status | Published - 1986 |
Externally published | Yes |