Fig. 14From: Use of ssq rotational invariant of magnetotelluric impedances for estimating informative properties for galvanic distortionCheckerboard structure with an anomaly size of 80 km \(\times\) 80 km and resistivities of 10 (dark gray) and 100 (light gray) \(\Omega \,{\text {m}}\). The checkerboard structure was embedded in the lower crust layer (from a depth of 14.8 to 33.3 km in the layered-earth model shown in Fig. 2a). Three arrays of 25 MT stations (crosses), each with a size of 160 km \(\times\) 160 km (dashed frames), were placed at central (black), northeast (blue), and northwest (red) positionsBack to article page