Fig. 7From: Magma reservoir beneath Azumayama Volcano, NE Japan, as inferred from a three-dimensional electrical resistivity model explored by means of magnetotelluric methodVertical profile of the final resistivity model in the N–S direction. The origin of the N–S coordinate is fixed at Oana Crater. Other features are the same as those in Figs. 5 and 6Back to article page