The Pangea/Laurasian supercontinent has undergone several unsuccessful attempts of
crustal break-up since late Devonian times. Early-middle Carboniferous, late Permian-early …

On the basis of sedimentary fill, tectonic style and crustal structure, the study area may be
divided into three main geological provinces, separated by major fault zones:(1) the oceanic …

The postglacial Quaternary colluvial systems in western Norway are arrays of steep fans,
often coalescing into aprons, developed along the slopes of valley sides and fjord margins …

Abstract The Norwegian Sea continental margin is dominated by two major basins with a
very thick Cretaceous basin fill: the Vøring and Møre Basins. The basins are flanked by 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 …

Abstract Information from multichannel seismic reflection data complemented by seismic
refraction, gravity and magnetics forms the basis for a regional structural and evolutionary …

A regional grid of multichannel seismic reflection profiles records the Late Palaeozoic
structure and tectonic development of the south-western Barents Sea. A 300 km wide rift …

Application of lineament analysis in structural geology gained renewed interest when
remote sensing data and technology became available through dedicated Earth observation …

Numerous reconstructions of the North Atlantic have been proposed based on fitting of
magnetic anomalies transform-fracture-zone systems, continent-ocean boundaries, and/or …

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 …