Address spatial continuity

Spatial continuity corresponds to the roughness factor of your main structure: in the case of a cubic variogram, the roughness
factor is small. It is recommended to select cubic variogram when your seismic time data set presents strong spatial continuity
between data values. Also, cubic variograms are very stable for kriging computations and very relevant for depth simulations.

For more information, see Variograms.

Spatial continuity corresponds to the roughness factor of your main structure: in the case of a spherical variogram, the roughness
factor is medium. It is recommended to select spherical variogram when your seismic time data set presents medium spatial continuity
between data values (i.e. the experimental variogram of the data exhibits linear behavior at the origin, appropriate for
representing properties with a medium level of short range variability).

For more information, see Variograms.

Spatial continuity corresponds to the roughness factor of your main structure: in the case of an exponential variogram,
the roughness factor is high. It is recommended to select Exponential variogram when your seismic time data set presents
low spatial continuity between data values (i.e. the experimental variogram of the data exhibits exponential behavior
at the origin, appropriate for representing properties with a high level of short range variability).

For more information, see Variograms.