Fig. 8From: Attenuation contrast in mantle wedge across the volcanic front of northeastern Japan that controls propagations of high-frequency S-wave later phasesExpected delay times of the scattered waves of backarc intraslab earthquakes, computed from the estimated passing points of the backarc earthquakes (Fig. 5) and forearc earthquakes (Fig. 7). Gray-filled symbols are the expected delay times in the cross-sections A–C. White symbols are the expected delay times in cross-sections D and E, and their temporal ranges corresponding to the 95% confidence intervals in the forearc region in Figs. 5 and 7Back to article page