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