1887

Abstract

A new theoretical model has been developed for transient controlled-source electromagnetic (CSEM) exploration of multi-layer aquifers. The method is applicable to fractured rock and other types of lithology which exhibit length-scale dependent heterogenity. A roughness parameter β is used, in the present paper, as a proxy for fracture density.

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/content/papers/10.3997/2214-4609-pdb.157.sageep021
2009-03-29
2021-01-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.157.sageep021
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