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Table 3 Models of the 1703 earthquake and tsunami. The parameters are as follows: d is focal depth, θ is strike, λ is slip angle, U is dislocation, L is fault length, and W is fault width

From: Source model of the 1703 Genroku Kanto earthquake tsunami based on historical documents and numerical simulations: modeling of an offshore fault along the Sagami Trough

Name

Mwa

Number of faults

Parameters of the offshore fault

References

d (km)

θ (deg)

δ (deg)

λ (deg)

U (m)

L (km)

W (km)

Model 1

8.33

3

0.0

300

30

135

7.1

100

50

Shishikura model in Satake et al. (2008)

Model 2

8.23

45

1.3

290

45

125

10

50

30

Namegaya et al. (2011)

Model 3

8.51

51,399

Cabinet Office (2013)

Model 4

8.30

45

1.3

290

45

125

20

50

30

This studyb

Model 5

8.30

45

1.3

290

45

125

10

50

60

This studyc

Model 6

8.32

45

1.3

274

45

109

10

120

30

This studyd

  1. aThe rigidity coefficient is 5 × 1010 Nm (Namegaya et al. 2011)
  2. bModel 2 × 2.0 fault slip factor (20 m slip)
  3. cModel 2 × 2.0 fault width factor (60 km width)
  4. dOffshore fault length of Model 2 was extended to 120 km along the Sagami Trough