Figure 6From: Imaging the hydrothermal system beneath the Jigokudani valley, Tateyama volcano, Japan: implications for structures controlling repeated phreatic eruptions from an audio-frequency magnetotelluric survey Comparison of pseudo-sections between the final 2D model responses (Figure 5 ) and the observed data. Left and right columns represent observed and calculated responses, respectively, with the upper chart showing TM-mode phase data and the lower chart showing TM-mode apparent resistivity data. Inverted triangles denote the AMT sites used for inversion (see Figure 1).Back to article page