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

* Maps and text (Introduction and Chapter 10) from AAPG Memoir 43, Evolution of the Arctic-
North Atlantic and the Western Tethys, by Peter A. Ziegler. Adapted here for online …

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 …

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 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 …

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 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 …

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

A tectono-magmatic model across the Vøring Plateau, NE Atlantic, has been derived from a
densely sampled ocean bottom seismic profile, constrained by multichannel seismic and …