Fig. 6
From: Deep structure and geothermal resource effects of the Gonghe basin revealed by 3D magnetotelluric
\({{\text{RMS}}}_{Update}\) of each magnetotelluric sounding station. a, b, c, d, respectively, represents the \({{\text{RMS}}}_{Update}\) value obtained by replacing the four adjacent layers of 24.75–28.23 km, 28.23–32.20 km, 32.20–36.72 km and 36.72–42.74 km in the resistivity model obtained by inversion with 100 Ω resistivity value in each station