Fig. 3From: Geometrical dependence on the stress and slip tendency acting on the subduction megathrust of the Nankai seismogenic zone off KumanoExample of picked reflection from the fault surface. (Left) Shallow section (seafloor to the bottom simulating reflector). (Right) Deep section (plate boundary fault and top of oceanic crust). By comparing with those from seafloor (positive), BSR (negative), and top of oceanic crust (positive), the picked fault has a negative polarityBack to article page