While there are numerous hypotheses concerning glacial–interglacial environmental and
climatic regime shifts in the Arctic Ocean, a holistic view on the Northern Hemisphere's late …

The continental margins surrounding the Norwegian–Greenland Sea are to a large degree
shaped by processes during the late Quaternary. The paper gives an overview of the …

A regional net erosion map for the greater Barents Sea shows that the different areas in the
Barents Sea region have been subject to different magnitudes of uplift and erosion. Net …

In the preceding chapters we have included only a few regional examples and case studies
because of space limitations. The present chapter will, however, provide some examples …

Palaeogeographic and tectono-stratigraphic considerations in the greater Barents Sea show
that the distribution of reservoirs and hydrocarbon source rocks from the Late Palaeozoic to …

The Barents Shelf, stretching from the Arctic Ocean to the coasts of northern Norway and
Russia, and from the Norwegian–Greenland Sea to Novaya Zemlya, covers two major …

A sequence stratigraphic framework of the Triassic on the Norwegian Barents shelf is
presented. The Triassic succession was subdivided into five second-order sequences based …

Ice can sculpt extraordinary landscapes, yet the efficacy of, and controls governing, glacial
erosion on geological timescales remain poorly understood and contended, particularly …

Trough mouth fans are fans at the mouth of transverse troughs/channels on glaciated
continental shelves. On the northwest European glaciated continental margin, eight trough …

Abstract The Norwegian Barents Sea with multiple source rock intervals represents a prime
example of an overfilled petroleum system. However, several episodes of uplift and erosion …