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Comments The area close to the margin of the East Shetland Platform and margin of the present Norwegian mainland shows generally a succession of sandstones and mudstones.

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A succession of a well which does not show a complete Triassic succession making it possible to subdivide it based on the overall lithostratigraphic pattern and totally absence of age diagnostic material makes it very difficult or impossible to decide which Triassic unit the sediments belong to.

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

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