
Due to the physics of the technique it is inherently better at detecting conductors in resistive environments rather than resistors in conductive environments. This technique is ideal for the detection and mapping of continuous, sub-surface, electrical conductors such as a massive sulphide orebody. It is also used for groundwater and environmental studies where the feature to be mapped is more conductive than its host. Examples of this would include water filled paleochannels or shear zones, saltwater incursion zones or mapping of leaking industrial waste.
Measurements are normally conducted at spacings
of 25 to 200 metres.


