J
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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Journal ArticleDOI
Late Weichselian and Holocene behavior of the Greenland Ice Sheet in the Kejser Franz Josef Fjord system, NE Greenland
TL;DR: In this paper , the late Weichselian and Holocene glacial history of a NE Greenland fjord system is reconstructed using new and previously published swath bathymetry and high-resolution seismic data, supplemented with multi-proxy analysis of sediment cores.
Journal ArticleDOI
Controlling factors for slope instability in a seismically active region: The NW-Svalbard continental margin
TL;DR: In this article, the authors describe the morphology and sedimentology of a slide area and discuss the potential trigger mechanisms that have led to multiple slope failure events along the NW-Svalbard margin, in close proximity to the tectonically active Spitsbergen Fracture Zone.
Book ChapterDOI
Submarine Glacigenic Debris Flows on the Bear Island Trough Mouth Fan, Western Barents Sea: Aspects of Flow Behaviour
Jan Sverre Laberg,Tore O. Vorren +1 more
TL;DR: In this paper, the authors investigated the flow behavior of large subaqueous debris flows on a low angle slope (< 1°) of the Bear Island Trough Mouth Fan (BIMF) in the western Barents Sea.
Book ChapterDOI
A Surging Behaviour of Glacigenic Debris Flows
TL;DR: Based on industry 3D seismic data, covering an area of 2,190 km2 of the continental slope offshore mid-Norway, the frontal part of glacigenic debris flow deposits have been studied as discussed by the authors.
Journal ArticleDOI
Submarine mass movements affecting contourites on the continental slope offshore of the Lofoten Islands, North Norway
TL;DR: The Lofoten drift as mentioned in this paper was formed by a series of submarine mass movements on the Norwegian continental margin during the last c.7 Ma, including high inputs of glacigenic sediments particularly beyond the mouths of ice streams.