Fig. 11From: Magma reservoir beneath Azumayama Volcano, NE Japan, as inferred from a three-dimensional electrical resistivity model explored by means of magnetotelluric methodPlan view of CRT as in Fig. 10, but using checkerboxes about 5 km to a side. The checkerboxes are embedded in the depth range from 5 to 10 km bsl, and the output models are shown at the depth of 7.5 km bslBack to article page