Elektromanyetik

Audio-magnetotelluric (AMT)

In the AMT (Audio-magnetotelluric) method, from among natural origin electromagnetic methods, the two- or three-dimensional map of the underground is obtained by the data collected at land, and the solutions of many problems are provided. It provides ease of application at rough lands compared to resistivity methods.

AMT method, that is able to provide information from the target depth in a short while, is effective in fields such as explorations of groundwater, geothermal resources and mine.

Magnetotelluric (MT)

In the MT (magnetotelluric) method, again from among natural origin electromagnetic methods, the two- or three-dimensional map of the underground is obtained by the data collected at land, and the solutions of many problems are provided. It provides ease of application at rough lands compared to resistivity methods.

It is sensitive to much deeper levels compared to AMT method. Thus, it requires a longer measurement period. It is a method frequently resorted to in especially deep geothermal researches such as crust studies, tectonic mechanism researches, deep structure researches, volcanic intrusions, superheated dry rock studies, nappe – base contacts.