Uplift and erosion are complex phenomena in terms of their governing processes, precise
timing and exact magnitude. The intricate relationship between different geodynamic …

Intraplate basin/structural inversion (indicating tectonic shortening) is a good marker of (“far-
field”) tectonic stress regime changes that are linked to plate geometries and interactions, a …

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 …

Abstract The Barents Sea is believed to have been influenced in most parts by Cenozoic
uplift and erosion episodes. The rocks in the area are not currently at their maximum burial …

A new generation of aeromagnetic data documents the post‐Caledonide rift evolution of the
southwestern Barents Sea (SWBS) from the Norwegian mainland up to the continent‐ocean …

Abstract The Middle to Late Triassic Snadd Formation represents one of the later stages of
Early Mesozoic infilling of the Barents Sea Basin, expressed by a silicilastic wedge …

Abstract From Permian to Jurassic times the northern Viking Graben and adjacent platform
areas experienced multiple rifting, the Permian-early Triassic and middle-late Jurassic rift …

Contractional structures (large anticlines and synclines, reverse faults and inverted centres
of deposition) of assumed Late Cretaceous–Cenozoic age are common in Cretaceous …

The juxtaposition of the North Atlantic rift system with the borderlands of the Eurasian Arctic
shelf has resulted in an unusual basin evolution in the southwestern Barents Sea …

Tectonic lineaments of the Norwegian mainland have been outlined and characterised in a
new lineament map of Norway. The underlay is a natio nal coverage of Landsat TM 7 …