The Atlantic margin of the Norwegian, Faeroese, British and Irish sectors encompasses
numerous basins which vary in character, but are related in terms of their evolution as part of …

Mangerites, charnockites, anorthosites, gabbros and granites occur within a high-grade
metamorphic complex in the Lofoten–Vesterålen islands of northern Norway. U–Pb dating of …

In this review we give an overview of geophysical data and models available for the
Scandinavian mountains and adjacent areas, as they are of relevance to the debate about …

The Tertiary development of the Norwegian continental margin was dominated by the
opening of the Arctic–North Atlantic Ocean. The correct identification of magnetic anomalies …

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 …

The Lofoten Ridge is a fault-controlled basement horst residing between Mesozoic basins
on the North Norwegian passive margin. This major horst and the adjacent offshore basin …

The Lofoten-Vesterålen continental margin (Fig. 1) marks the transition between the much
wider, passive continental Møre-Vøring margin (Blystad et al. 1995; Brekke 2000) and the …

Major crustal units in the western Barents Sea have been defined on the basis of depth‐
converted seismic reflection data, gravity and magnetic anomaly data. The seismic data …

A north to northwest trending mafic dyke swarm of gabbronoritic and gabbroic composition
makes up a significant part of the Archean basement on the island of Ringvassøy in northern …

We have utilised potential field data in combination with seismic interpretation and bedrock
mapping to improve the understanding of basement structures and rifting processes on the …