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Figure 1 – Panel a) shows a time slice of seismic data containing channels, and b) shows a vertical slice of the same seismic data taken perpendicular to the paleo-flow of the channels. Three channels – a, b and c – are identified. Panels c) and d) show the instantaneous frequency attribute for the views shown in a) and b), respectively. These images suggest frequencies in the 40-60 Hz range are likely associated with the channels.
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Figure 1 – Panel a) shows a time slice of seismic data containing channels, and b) shows a vertical slice of the same seismic data taken perpendicular to the paleo-flow of the channels. Three channels – a, b and c – are identified. Panels c) and d) show the instantaneous frequency attribute for the views shown in a) and b), respectively. These images suggest frequencies in the 40-60 Hz range are likely associated with the channels.