Permafrost mapping by audiofrequency magnetotellurics

The audiofrequency magnetotelluric (AMT) method has been used to study permafrost thickness near Tuktoyaktuk, N.W.T. in the Mackenzie Delta. In the frequency range of 10 Hz–10 kHz the permafrost behaves as a simple resistive layer over a conductive layer. This simple two-layer model can be inverted...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Koziar, A., Strangway, D. W.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1978
Subjects:
Online Access:http://dx.doi.org/10.1139/e78-159
http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-159