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Fig. 3 | Earth, Planets and Space

Fig. 3

From: Source model of the 1703 Genroku Kanto earthquake tsunami based on historical documents and numerical simulations: modeling of an offshore fault along the Sagami Trough

Fig. 3

Previously proposed source models of the 1703 earthquake and resulting tsunami. a Model 1 (Shishikura model in Satake et al. 2008). b Model 2 (Namegaya et al. 2011). c Model 3 Cabinet Office (2013). The area of Model 3 is divided into 100 segments to determine the fault slip parameter. These segments are further divided into 51,399 nodes to extract the other fault parameters, such as the fault depth, strike and dip angle (also see Table 3)

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