Image Gallery

Figure 1 – Vertical slices through a 3-D seismic volume showing a targeted channel system (a) and horizon slices A, B, C and D, which cut through the channel window (b). These four horizon surfaces are approximations to stratal surfaces because they are conformable to the indicated reference surface, which is a chronostratigraphic reflection event. This profile is labeled 200 on figure 2.
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Figure 1 – Vertical slices through a 3-D seismic volume showing a targeted channel system (a) and horizon slices A, B, C and D, which cut through the channel window (b). These four horizon surfaces are approximations to stratal surfaces because they are conformable to the indicated reference surface, which is a chronostratigraphic reflection event. This profile is labeled 200 on figure 2.