Thirty years of research, and especially the refinements of many geological, geochemical
and geophysical techniques, have uncovered many new facets of the geology of the …

Eocene magmatic breakup along the mid‐Norway rifted margin was preceded by extreme
Jurassic‐Cretaceous crustal thinning in a magma‐poor environment. Along the SE borders …

Abstract The Geological Survey of Norway (NGU) has produced new aeromagnetic and
gravity maps from Norway and adjacent areas, compiled from ground, airborne and satellite …

Detachment fault systems typically record displacements in the order of 10s of kilometers.
The principles that control the growth of smaller magnitude normal faults are not fully …

Based on observations from the Mid-Norwegian extensional system, we describe how, when
and where the post-Caledonian continental crust evolved from a context of orogenic …

The large‐magnitude faults that control crustal thinning and excision at rifted margins
combine into laterally persistent structural boundaries that separate margin domains of …

Thrust sheets of the Uppermost Allochthon in the Caledonides of Scandinavia are
distinguished by lithological assemblages and magmatic units that are, in many ways, quite …

The (ultra) high-pressure Western Gneiss Region of the Norwegian Caledonides represents
an archetypical orogenic infrastructure of a continent–continent collision zone. To test …

Structures related to orogenic “collapse” may provide an important template for reactivation
during later rifting. In the proximal rifted margin offshore Norway, the tectono‐sedimentary …

Basement fracture and fault patterns on passive continental margins control the onshore
landscape and offshore distribution of sediment packages and fluid pathways. In this study …