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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 layerVp [km/s]Vp [km/s]ρ [g/cm3]H [km]
Source31.500.001.006.0
 6.003.502.706.0
 8.104.703.30Half space
Receiver36.003.502.7018.0
 6.753.802.8018.0
 8.104.703.30Half 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