Skip to main content
Earth, Planets and Space
Fig. 6 | Earth, Planets and Space

Fig. 6

From: Attenuation contrast in mantle wedge across the volcanic front of northeastern Japan that controls propagations of high-frequency S-wave later phases

Fig. 6

Estimated locations of passing points at cross-sections D and E in four models: a, e the HH2010 model, a layered model with velocities used in Hasemi and Horiuchi (2010). b, f The WoQ model, excluding attenuation effects. c, g The HighQ model: assuming weak attenuation (\({Q}_{\mathrm{S}}=300\)) in the backarc mantle wedge (gray-shaded area). d, h The LowQ model, assuming strong attenuation (\({Q}_{\mathrm{S}}=100\)) in the backarc mantle wedge. The attenuation structure in the HH2010 model and the velocity structure in the WoQ, HighQ, and LowQ models are the same those shown in Fig. 4. Other symbols are explained in the caption of Fig. 5

Back to article page