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  | isbn    = 0-89181-602-X

  | isbn    = 0-89181-602-X

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Below is a recipe for making a classic integrated structure map from seismic data and well control. It is based on mapping one horizon at a time and must be repeated for each horizon of interest. It may not work in areas with severe static problems (i.e., lots of topography or a rapidly changing weathered layer such as glacial till). It also fails when there are extreme lateral velocity variations in the subsurface (subsalt, subthrust, etc.). When it works, this method gives a map which, by definition, matches every well exactly. It uses seismic time structure to interpolate between wells and extrapolate beyond them.

Below is a recipe for making a classic integrated structure map from seismic data and well control. It is based on mapping one horizon at a time and must be repeated for each horizon of interest. It may not work in areas with severe static problems (i.e., lots of topography or a rapidly changing weathered layer such as glacial till). It also fails when there are extreme [[lateral]] velocity variations in the subsurface (subsalt, subthrust, etc.). When it works, this method gives a map which, by definition, matches every well exactly. It uses seismic time structure to interpolate between wells and extrapolate beyond them.

==Procedure==

==Procedure==