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The Group is thinning towards the west in the northernmost part of the northern North Sea while in the southern part Central Trough and Moray Firth substantial thicknesses are recognized.

The following Norwegian wells are used to illustrate the Group: , and.

Thickness The Hegre Group is thickest in the eastern part of the basin where major subsidence occurred along the present Norwegian coastline.

The actual succession should therefore be assigned unspecified to the Hegre Group.

The Cormorant Formation is therefore here suggested to be abandoned.

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Type area The type area is the northern part of the northern North Sea.

It represents a transition from high gamma and sonic readings of the carbonate dominated Zechstein facies to low gamma and sonic of the Smith Bank Formation.

There might have been depositional systems along the East Shetland Platform during deposition of the Hegre Group as great thicknesses of unspecified Triassic strata have been drilled here see Comments below.