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Here, we assume that each of the wave packets S1 S4 are generated from individual strong motion generation areas, SMGA1 SMGA4.
Two strong motion generation areas are identified in the Miyagi-oki region west of the hypocenter.
All the strong motion generation areas exist in the deeper portion of the source fault plane.
Such origins are considered to be the strong motion generation areas (SGMAs).
Another two strong motion generation areas (SMGA3 and SMGA4) are located in the Fukushima-oki region southwest of the hypocenter.
Figure 1 shows the distribution of strong motion generation areas (SMGAs) according to several recent source models.
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Source characterization for broadband ground-motion simulation: Kinematic heterogeneous source model and strong motion generation area.
In this study, using the EGFM, we estimate the strong motion generation area (SMGA) and the stress drop by sequence.
The strong motion generation area (SMGA) models of Kamae and Kawabe (2004) and Morikawa et al. (2006) are also referred to determine the approximate locations of the asperities.
Miyake et al. (2003) named this source patch the strong motion generation area (SMGA), and this is defined as the area characterized by a large uniform slip velocity within the total rupture area, which reproduces near-source strong ground motions up to about 10 Hz.
The strong motion generation area and the empirical Green's function method has been successfully applied to strong motion simulations of past subduction-zone in-terplate earthquakes (e.g., Kamae and Kawabe, 2004; Miyahara and Sasatani, 2004; Suzuki and Iwata, 2007; Takiguchi et al., 2011).
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