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The migration velocity model (provided by Norsk Hydro), shows a large, complex salt body with
steeply dipping flanks in both
inline and cross-line directions (Figure 5). The water-bottom itself dips
in some places as much as 11 degrees in the cross-line direction, although it is
relatively flat in the inline direction.
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vmodel
Figure 5. Subsurface velocity model. Note the strong dips in both
the inline and cross-line directions.
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2007-10-24