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Fault model of the 2007 Noto Hanto earthquake estimated from coseismic deformation obtained by the distribution of littoral organisms and GPS: Implication for neotectonics in the northwestern Noto Peninsula

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Figure

Fig. 1.Distribution of active faults (Research Group for Active Faultsin Japan, 1991; Katagawa et al., 2005; GSJ, 2007a), geological faults(GSJ, 2005), and aftershocks (M ≥ 2) (circles) within 1 day after themainshock reported by JMA
Fig. 2. A temporal variation in the distribution of the aftershocks (M ≥ 2) of the Noto Hanto earthquake (a) during 1 h and (b) during 1 day after theearthquake
Fig. 4. Distribution of the sites of the measurements of coseismic verticalcrustal deformation using the distribution of littoral organisms alongthe coast (triangles) of the northern Noto Peninsula
Fig. 5. Schematic views of (a) the biological vertical zonation of the littoral area in the Noto Peninsula (modified after Raffaelli and Howkins, 1996) and(b) analytical methods of this study
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