On the detection of geologically complex areas by the radio-wave transmission method in stratiform deposit mining

Abstract

In general, geologically complex areas of stratiform deposits represent zones of faults that differ slightly in electrical properties from the well-conducting surrounding rocks. To study faults located in a highly conductive medium and at considerable (up to 200 m) distances from the source of electromagnetic waves, relatively low frequencies are required, and it is often impossible to use conventional methods of interpreting the results of radio-wave transmission.

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