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Seismotectonic implications of the Kyushu Palau ridge subducting beneath the westernmost Nankai forearc

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Figure

Fig. 1. Bathymetry map and locations of MCS (black thin; this study) and OBS (black dotted; Ichikawa, 1997) lines in the westernmost Nankai Troughmargin off southwest Japan
Fig. 2. Prestack depth migrated MCS profile on line KR0114-8 showing the subducted Kyushu-Palau ridge
Fig. 4. Schematic diagram illustrating the proposed locally large stress zone (light pink ellipse) and slab fracture (heavy blue dotted line) caused bythe Kyushu-Palau ridge subduction (thin red dotted line)

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