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Abstract

When surveying upon a level homogenous halfspace or over borizontally layered lithologies no anomalies are seen in the conventional VLF-EM method. But in situations where the topography represents a surface with varying relief even upon a homogenous halfspace the terrain itself will generate VLF-EM anomalies which can be misinterpreted as originating from subsurface conductors.

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/content/papers/10.3997/2214-4609.201407346
1997-08-09
2021-04-21
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407346
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