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Abstract

The Geological Survey of Norway has developed a method for recognizing lateral resistivity inhomogeneities with the Schlumberger cable (Ronning and Tønnesen 1990). The equipment used is constructed at the Geological Survey of Norway and consists of a multicore cable system. In this system the current and potential electrodes are connected to separate cables in order to avoid current leakage in the connections and cables.

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/content/papers/10.3997/2214-4609.201411532
1993-06-08
2025-04-22
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