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Progress in Earth and Planetary Science
Fig. 12 | Progress in Earth and Planetary Science

Fig. 12

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

Fig. 12

Example of time-migrated MCS sections after flattening by the basement (top of the oceanic crust) reflection picks. The processing flow is the same as in Fig. 10, and the line positions are shown in Fig. 1. The blue line segments are the interpreted Moho, showing the thickness of the oceanic crust. The dashed red line plotted at 2.0 s is a reference line for variations in the crustal thickness along the profile. See the supplementary materials for more examples

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