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Jan Sverre Laberg

Researcher at University of Tromsø

Publications -  138
Citations -  6712

Jan Sverre Laberg is an academic researcher from University of Tromsø. The author has contributed to research in topics: Continental margin & Continental shelf. The author has an hindex of 44, co-authored 128 publications receiving 6140 citations.

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The Andøya Slide and the Andøya Canyon, north-eastern Norwegian–Greenland Sea

TL;DR: Based on GLORIA side-scan sonar imagery, echo sounder records, 3.5 kHz profiles, multichannel seismics and gravity cores the Andoya Slide and Andoya Canyon, north-eastern Norwegian-Greenland Sea were mapped and interpreted.
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Seismic analyses of Cenozoic contourite drift development in the Northern Norwegian Sea

TL;DR: In this article, four drift accumulations have been identified on the continental margin of northern Norway; the Lofoten Drift, the Vesteralen drift, the Nyk Drift and the Sklinnadjupet Drift.
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Late Quaternary glacial development of the mid-Norwegian margin—65 to 68°N

TL;DR: In this article, the younger part of the large Plio-Pleistocene prograding wedge on the northern half of the mid-Norwegian margin was studied using high-resolution seismic data.
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Flow behaviour of the submarine glacigenic debris flows on the Bear Island Trough Mouth Fan, western Barents Sea

TL;DR: In this paper, the authors used 3·5 kHz high-resolution seismic data, gravity cores and side-scan sonar imagery to study the flow behavior of submarine, glacigenic debris flows on the Bear Island Trough Mouth Fan, western Barents Sea.
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Neogene evolution of the Atlantic continental margin of NW Europe (Lofoten Islands to SW Ireland): anything but passive

TL;DR: A regional stratigraphic framework for the Neogene succession along and across the NW European margin is presented, based on a regional seismic and sample database as discussed by the authors, which provides constraints on the timing and nature of the mid-to late Cenozoic differential tectonic movements that have driven major changes in sediment supply, oceanographic circulation and climate (culminating in continental glaciation).