Resistivity Method (CS - apparent resistivity method)
This method is based on studying the heterogeneity of the specific electrical resistivity within rock formations. The resistance of the layers depends on factors such as the presence of water, its salinity, the composition of the rocks, their structure, and porosity. It is widely used for exploration and mapping purposes
Induced Polarization (IP) method
It is based on the redistribution of charges in rocks when the current is turned on and off. It allows simultaneous measurement of polarization and apparent resistance. This method is used for the detection of ores with vein-like or disseminated sulfide mineralization, graphite bodies, and groundwater.
A probing technique for studying the distribution of geoelectrical properties at depth. The results are displayed as cross-sections or 3D models of polarizability and resistivity, allowing for precise investigation of the subsurface structure.
A technique aimed at studying the variability of geoelectrical properties across an area. It involves measuring both resistivity and polarizability. The result is a VP or CS map, which helps identify promising zones for further investigation.
