Electricity

Self-Potential Method

In SP method, from among natural origin methods, the data obtained at land is presented graphically or as surface cross-section following mathematical corrections. It can be used in the determination of faults and grikes close to surface, in exploration of sulphur ore and groundwater, and at geothermal sites.

Resistivity Method

It is among the geophysical methods extensively used today. The two or three dimensional maps of the underground are obtained by the data collected at land, and the solutions of many problems are provided. It provides effective results in fields such as groundwater and geothermal resource searches, mine searches, archeological researches, and ground strength and landslide researches.

Induced Polarization Method

It is a successful geophysics method in sulphide mine explorations. Greatly effective results are obtained as being applied along with the resistivity method. Again, the two or three dimensional electric and chargeability maps of the site, where it is applied, may be obtained.