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Figure 16 Contrast functions G for depth source localization by TFa approach.
Figure 20 Contrast functions G for depth source localization by F-K approach.
Figure 22 Contrast functions G for depth source localization by F-K approach combined with source spectrum estimation.
The vertical resolution is 5 m. Figure 17 Contrast functions G for depth source localization by TFa approach with false mode sign estimation.
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They concluded that the oceanic layer has a large influence on the Rayleigh waves for a shallow (∼5-km depth) earthquake, whereas it has negligible influence on synthetic seismograms for a deep (> 10-km depth) source.
To summarize, we conclude: 1. Amplitudes of fundamental mode of Rayleigh waves, which are generated by shallow (around 5 km in depth) sources, are larger for the model without the oceanic water layer than for the model with the oceanic water layer.
Euler deconvolution is an automated function for determining the depth to source from profiles.
The same goes for depth of field.
Tone and tact substitute for depth.
For depth.
Add shadows for depth.
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