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Table 2 Parameters in our best simulation model at points 1–12 in Fig. 4e, f

From: Simulation of great earthquakes along the Nankai Trough: reproduction of event history, slip areas of the Showa Tonankai and Nankai earthquakes, heterogeneous slip-deficit rates, and long-term slow slip events

Point (Fig. 4e, f)

L (m)

σeff (MPa)

h* (km)

a

b

a–b

1

0.4000

40

100.0

0.005

0.008

− 0.003

2

0.2200

35

62.9

0.005

0.008

− 0.003

3

0.0800

30

26.7

0.005

0.008

− 0.003

4

0.1700

30

56.7

0.005

0.008

− 0.003

5

0.6000

40

150.0

0.005

0.008

− 0.003

6

0.2400

60

40.0

0.005

0.008

− 0.003

7

7.5000

30

2500.0

0.005

0.008

− 0.003

8

0.0150

5

30.0

0.005

0.008

− 0.003

9

0.0335

10

33.5

0.005

0.008

− 0.003

10

0.0335

10

33.5

0.005

0.008

− 0.003

11

0.0335

10

33.5

0.005

0.008

− 0.003

12

7.5000

30

–

0.005

0.002

0.003