Jan Sverre Laberg

TL;DR: In this article, a 3D reflection seismic imaging technique was used to identify large-scale submarine geomorphic features produced by former ice sheets, including elongated ridge-groove features, interpreted to be glacial bedforms produced by fast-flowing grounded glaciers.

TL;DR: In this article, a regional correlation of Neogene stratigraphy has been attempted along and across the NW European Atlantic continental margin, between Mid-Norway and SW Ireland, and two unconformity-bounded successions are recognized.

TL;DR: In this article, the Cenozoic history of post-rift vertical movements along the NW European margin, from Ireland to mid-Norway, is examined by integrating published analyses of uplift and subsidence with higher resolution tectono-stratigraphic indicators of relative movements.

TL;DR: Based on studies of sediment accumulations deposited from-and erode by-alongslope flowing ocean currents on the European continental margin from Porcupine (Ireland) to Lofoten (Norway), the evolution of the Cenozoic paleocirculation was reconstructed as part of the STRATAGEM project as mentioned in this paper.

TL;DR: In this paper, the main building blocks of deep-sea fans along the Norwegian-Barents Sea continental margin were found to have been formed by the input of clay-rich sediments to the upper continental slope by glaciers during periods of maximum ice advance.