Abstract The North Atlantic, extending from the Charlie Gibbs Fracture Zone to the north
Norway-Greenland-Svalbard margins, is regarded as both a classic case of structural …

Collision between Baltica and Laurentia in Siluro Devonian time resulted in a stack of thrust
sheets, the Caledonides of Scandinavia and East Greenland, which were amalgamated and …

Following an outline of Scandinavian Caledonide tectonostratigraphy, tracing the
Neoproterozoic, Baltoscandian, passive margin of Baltica outboard into the suspect, Iapetus …

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 …

The late Silurian to mid-or late Devonian interval in the Caledonides was a period
dominated, sequentially, by sinistral transpression, strike-slip and transtension during the …

Extensional structures characterize significant parts of the North Atlantic Caledonides.
Silurian extensional deformation took place, particularly in the heated crust in the southern …

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 …

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 …

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