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Fig. 10 | Progress in Earth and Planetary Science

Fig. 10

From: Numerical estimation of a tsunami source at the flexural area of Kuril and Japan Trenches in the fifteenth to seventeenth century based on paleotsunami deposit distributions in northern Japan

Fig. 10

Seismological characteristics in Hokkaido and Tohoku regions. a The interplate earthquakes occurring from 1984 to 2013 CE compiled by Nakamura et al. (2016), b the distribution of slip deficit, compiled by Suwa et al. (2006), and slow earthquake distributions, compiled by Nishikawa et al. (2019). The black and viridis-color lines in a represent contour with a 10 m slip interval of the 2011 Tohoku-oki tsunami by Iinuma et al. (2012) and with a 1 m slip interval of the 1968 CE Tokachi-oki tsunami by Nagai et al. (2001), respectively. The slip deficit is estimated from three-dimensional global positioning system velocity data from 1997 to 2001 CE by Suwa et al. (2006). The white stars indicate the epicenters of historical earthquake (see Table 1 for detail). The viridis-color bar in a shows the slip amount; yellow is large, and purple is small. The white circles in b show the epicenters of tectonic tremor occurrence from August 2016 to August 2018. The light green circles in b denote the epicenters of very-low-frequency earthquakes from January 2005 to August 2018 CE. These data refer directly to the original supplement data in Nishikawa et al. (2019). The red star in b shows the main shock epicenter of the 2011 CE earthquake. The black circles in a and b indicate the explainable sites by the S2 model. The dark pink frame in a and b shows the rupture area of the S2 model

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