Abstract
An analogue model for studying the behavior of the natural geomagnetic and telluric field variations for various geological structures is described. Measurements of amplitudes and phases for the horizontal electric, the horizontal magnetic, and the vertical magnetic field components are obtained and discussed for various conducting vertical faults and dykes for both the H and the E polarizations.
Publisher
Canadian Science Publishing
Subject
General Earth and Planetary Sciences
Cited by
11 articles.
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