Abstract Based on a brief description of the geological background of the ore district, his paper
mainly analyses electrical anomaly properties and ground electric profile features along No.0 line in the
ore district by using the complex resistivity method. The horizontal projection shape of ore (mineralized)
bodies in the depth are illustrated by application of data from complex resistivity method in
combination with a discussion of stratigraphic and metallogenic conditions. Geophysical interpretation
played a guiding role in subsequent detailed exploration and was consistent with the drilling results.
The complex resistivity method proves to be a practical and efficient technique.
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