Fig. 18From: Magma reservoir beneath Azumayama Volcano, NE Japan, as inferred from a three-dimensional electrical resistivity model explored by means of magnetotelluric methodLow viscosity ellipse model (enclosed by broken line) by Takada and Fukushima (2013), and Mogi source locations of the two (solid circle) or three (solid star) inflation source models by Seki et al. (submitted to Quart. J. Seismology) superimposed on the N–S vertical profile of the final resistivity model (H'–H profile in Fig. 7)Back to article page