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Volume 25 Number 2
  • E-ISSN: 1365-2478

Abstract

A

Telluric current measurements in the audio and sub‐audio frequency range, made in various parts of Canada and South America over the past four years, indicate that the signal amplitude is relatively uniform over 6–8 midday hours (LMT) except in Chile and that the signal anisotropy is reasonably constant in azimuth.

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/content/journals/10.1111/j.1365-2478.1977.tb01172.x
2006-04-27
2024-04-26

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References

  1. Innes, M. J. S., and Argun‐Weston, A., 1967, Gravity measurements in Appalachia and their structural implications in Appalachian tectonics, Royal Society of Canada Special Publication #10, Univ. of Toronto Press.
    [Google Scholar]
  2. Slankis, J. A. and Becker, A., 1969, Telluric and magnetotelluric measurements at 8 Hz, AIME Trans.244, 237–244.
    [Google Scholar]
  3. Slankis, J. A., Telford, W. M., and Becker, A., 1972, 8 Hz telluric and magnetotelluric prospecting, Geophysics37, 862–878.
    [Google Scholar]
  4. Ward, S. H., 1967, in Mining Geophysics2, 249–274, Tulsa , Society of Exploration Geophysicists.
    [Google Scholar]
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  • Article Type: Research Article

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