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Reexamination of the fault slip model of the 1891 M 8 0 Nobi earthquake: The first earthquake detected by a geodetic survey in Japan

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Figure

Fig. 1.Location map of the triangulation network and leveling routes for the 1891 Nobi earthquake, as discussed in this study
Fig. 2. Observed and calculated coseismic deformation of the 1891 Nobiearthquake at the triangulation stations and benchmarks
Table 1.Fault parameters. Latitude and longitude represent vertical projections of the north corner of the upper edge of the fault onto the Earth’ssurface
Fig. 5. Location of the best fault models (dashed lines) in cross-sections AB in Fig. 4 relative to the location of earthquakes with intensities M > 0.0recorded from October 1998 to 2007 (indicated by circles).

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