Figure 3From: Long-period ground motions in a laterally inhomogeneous large sedimentary basin: observations and model simulations of long-period surface waves in the northern Kanto Basin, Japan Spatial variations of V 0 and α in the initial model. The values for V 0 and α were constructed by the interpolation of 15 local S-wave velocity structures (Yoshimoto and Takemura 2014a).Back to article page