Changes

  | isbn    = 0-89181-602-X

  | isbn    = 0-89181-602-X

}}

}}

[[file:exploring-for-stratigraphic-traps_fig21-4.png|left|thumb|{{figure number|1}}. Copyright: Sarg, 1988; courtesy SEPM.]]

[[file:exploring-for-stratigraphic-traps_fig21-4.png|left|thumb|{{figure number|1}}. Copyright: Sarg, 1988; courtesy SEPM.]]

Correlations with well data, such as cuttings, cores, or well logs, can be done to a much higher resolution than seismic scale correlations. The scale of a seismic wavelet limits the scale of correlations within a seismic section. The geologist must refine these correlations to a higher resolution using well data to more accurately define the location of seals and reservoirs.

Correlations with well data, such as cuttings, cores, or well logs, can be done to a much higher resolution than seismic scale correlations. The scale of a seismic wavelet limits the scale of correlations within a seismic section. The geologist must refine these correlations to a higher resolution using well data to more accurately define the location of seals and reservoirs.