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Progress in Earth and Planetary Science

Table 3 Velocity structure used for the teleseismic calculationa

From: Fault model of the 2012 doublet earthquake, near the up-dip end of the 2011 Tohoku-Oki earthquake, based on a near-field tsunami: implications for intraplate stress state

Structure

# of layer

Vp [km/s]

Vp [km/s]

ρ [g/cm3]

H [km]

Source

3

1.50

0.00

1.00

6.0

 

6.00

3.50

2.70

6.0

 

8.10

4.70

3.30

Half space

Receiver

3

6.00

3.50

2.70

18.0

 

6.75

3.80

2.80

18.0

 

8.10

4.70

3.30

Half space

  1. aThe structure is based on Kikuchi and Kanamori (1991) but the water layer (thickness of 6 km) is assumed for the source structure
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