4 Result(s)
within
Chapter
J. S. Laberg
Fossil Fuels (incl. Carbon Capture)
Geophysics/Geodesy
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Chapter
The Trænadjupet Slide: Sediment Disintegration and Flow
The Trænadjupet Slide is located on the continental slope of Norway immediately NE of the Vøring Plateau (Dowdeswell et al. 1996). The slide-affected area extends from the shelf break to >3,000 m water depth in t...
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Chapter
Morphology of the Lofoten Basin Channel
A deep-sea channel system, the Lofoten Basin Channel, has been identified in the SE Lofoten Basin (Dowdeswell et al. 1996; Vorren et al. 1998). The channel represents the downslope continuation of the Andøya Cany...
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Chapter
Submarine Glacigenic Debris Flows on the Bear Island Trough Mouth Fan, Western Barents Sea: Aspects of Flow Behaviour
The Bear Island Trough Mouth Fan is situated in front of the Bear Island Trough in the western Barents Sea. The fan extends from the shelf break to water depths greater than 3,000 m and covers an area of appro...
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Chapter
The Lofoten Contourite Drift: High-Resolution Seismic Stratigraphy
A contourite drift, the Lofoten Drift, has been identified from ca. 1,000 m water depth on the continental slope off northern Norway (Laberg et al. 1999) (Fig. 1). The Norwegian Current transporting Atlantic wate...
