Abstract

Electrical resistivity method consist of various arrays that had been successfully applied in mineral explorations. Three important electrode arrays in 2D imaging surveys were tested in this study by creating a tomography of the subsurface to determine which array is the most successful in defining the cassiterite bearing layer. These arrays are Wenner, Schlumberger and Dipole - dipole. The numerical modeling was created through vertical fracture zone and correlated with a representative lithology of the area produced by using tape to measure depths to different lithology at an exposed mining pit. The results showed that the Schlumberger is the most suitable electrode array that can resolve both vertical and horizontal structures present in the subsurface. It was also obvious that the Schlumberger is a better array that images the vertical and horizontal contacts and represented these geological structures more accurately than the Wenner and Dipole-dipole arrays.

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