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Abstract

Measurements with electric and electromagnetic methods on the Earths surface have a limited capability of resolving the conductivity structure of the ground. Thin layers that are not individually resolved will cause an apparent anisotropy - macro anosotropy - of an interpreted layer.

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/content/papers/10.3997/2214-4609.201410704
1992-06-01
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410704
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