Magnetotelluric (MT) method is an important passive surface geophysical method which uses the Earth’s natural electromagnetic fields to investigate the electrical resistivity structure of the subsurface and determines the resistivity distribution of the earth. Static shift is one of disorders arising from shallow conductors that can lead to severe problems in the interpretation of magnetotelluric (MT) data by shifting the MT apparent resistivity sounding curve. Therefore, static shift must be corrected as one of MT data processing steps. In this paper to show the application of determinant data, we present a case study and use the determinant data as an effective replacement for the static shift correction.