Fig. 17From: Magma reservoir beneath Azumayama Volcano, NE Japan, as inferred from a three-dimensional electrical resistivity model explored by means of magnetotelluric methodVertical profiles of the Vs model by Okada et al. (2015) superimposed on the resistivity model (Fig. 7) in the N–S direction. Other features are the same as those in Figs. 7 and 16Back to article page