Seismic refraction measurements and continuous seismic profiling on the continental margin off Norway between 60°N and 69°N.
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The sedimentary basin off Norway wedges out near the Norwegian coastline. The ocean side of the sedimentary basin is in contact with oceanic crust along escarpments and the Jan Mayen Fracture Zone. The present study reveals that the contact zone between the crust of oceanic and continental origin on the continental margin may be very complex and difficult to identify confidently on the basis of work carried out to date.