Abstract
Multichannel seismic reflection measurements off Lofoten, Northern Norway," "show an uneven, discontinuous reflector within the crystalline oceanic crust" "at a depth of 7-8 s (two-way traveltime). This intra-oceanic crustal reflector" "is observed seaward as well as beneath sub-basement dipping reflectors, which" "are of disputed (oceanic or continental) origin. Our observations indicate that" "the dipping reflectors are an integrated part of the oceanic crust.
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