Fig. 16From: 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. 6) in the E–W direction. The white lines and circles are Vs contours and sampling point of the Vs model. Other features are the same as those in Fig. 6Back to article page