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Abstract

The VLF technique has been applied during the past several decades for mapping of large areas with special regard to fracture zones, which typically transect the rocks as moderately resistive parts in an otherwise rather insulating background. Mapping with the VLF technique produces a detailed image of the subsurface conductivity structure of the measured area .

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/content/papers/10.3997/2214-4609.201410561
1992-06-01
2024-04-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410561
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