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A sequence stratigraphic subdivision of the upper Paleocene and the Oligocene is used to exemplify the influence of regional tectonism, local tectonism and climatic changes onto sedimentation in an epicontinental basin.The analysis shows that the low sedimentation rate and the condensed character of the Paleocene sediments disable any identification of climatic changes, whereas the Oligocene sequence boundaries are controlled by glacio-eustatic sea level changes. Regional tectonism played a major role in generating areas exposed for erosion located east of the present North Sea Basin.These exposed areas generated sand rich mass flows during the late Paleocene and generated the large amount of sediments which prograded into the Norwegian-Danish Basin during the Oligocene Local tectonics controlled generation of topographic depressions in the western part of the Norwegian-Danish Basin. The subtle depressions controlled the location of the sand rich mass flow deposits both during the late Paleocene and the latest Oligocene.

Tectonic vs climatic control on the sequence development, examples from the Paleogene succession in the eastern North Sea area