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Abstract

For the achievement of more efficient detection and determination of geological structures and sub-surface inhomogenities, a focusing four-electrode current arrangement has been developed - Fig 1. This arrangement does not include potential electrodes. Measurement is performed by three ampermeters and a voltmeter. The ampermeters measure the current intensities of corresponding electrodes, whereas the voltmeter controls the potential difference between the electrodes.

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/content/papers/10.3997/2214-4609.201411524
1993-06-08
2024-04-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201411524
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