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Earthquake Source Characterization Through Seismic Observations and Numerical Modeling

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Figure

Figure 2.2: Earthquakes at the downdip edge of the Tohoku-Oki rupture region.These seismic events have displayed very similar focal mechanism and waveformcomplexity
Figure 2.3: Comparison between 1D (marked in red) and 3D (marked in black)selected are between the azimuthal range of 240synthetic waveforms of event E1
Figure 2.4: (Left) Stations (triangles) are colored by the cross-correlationtime-shift value to align the data and synthetics, ranging from -4 to 4 seconds, withpositive value representing faster synthetics
Figure 2.6: Comparison of focal mechanisms from CAP inversion. (a) CAP inversionof E1 waveform data (bandpass filter applied from top to bottom: up to 20s, 10s,4s, and 1s) at F-net station KSN
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