Fig. 2From: Imaging of a serpentinite complex in the Kamuikotan Zone, northern Japan, from magnetotelluric soundingsExamples of sounding curves of apparent resistivity and impedance phase. Solid circles with error bars are observed impedances. Note that the error bars include error floors (see Sect. “3-D electrical resistivity inversion” for details). Solid lines are the responses of the inverted resistivity model and dashed lines are those for the sensitivity test model in which the C-2 anomalous zone (see Fig. 3) was assigned an apparent resistivity of 100 Ω m (see Sect. “Sensitivity test for resistivity anomalies”)Back to article page