Figure 3From: Seismic activity near the Moriyoshi-zan volcano in Akita Prefecture, northeastern Japan: implications for geofluid migration and a midcrustal geofluid reservoirVelocity models used for the location of hypocenters. Blue and red lines show the models used for the homogeneous station method (Figure 2b and Figure 4b) and for the hypoDD location. We used several values for the surface layer to assess the uncertainty of the hypocenter location.Back to article page