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Progress in Earth and Planetary Science
Fig. 13 | Progress in Earth and Planetary Science

Fig. 13

From: The nature of the Pacific plate as subduction inputs to the northeastern Japan arc and its implication for subduction zone processes

Fig. 13

Map of the crustal thickness in two-way time derived from all the MCS lines shown in Fig. 1. The processing flow was the same as in Fig. 10. Note that the crustal thickness could be mapped only the area where we could identify both basement and Moho reflections. The seafloor topography was plotted in grayscale, and water depth contour lines were plotted as the thin black line every 200 m. The thick contour line corresponds to a 5400 m water depth, showing the approximate extent of the Hokkaido Rise (Kobayashi et al. 1998)

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