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• W1981197993 abstract "Abstract Seismic refraction and continuous reflection measurements were made in the southern Barents Sea. On the basis of these investigations and earlier data from the area, the total thickness of sediments and thickness of the semiconsolidated section have been mapped. The main part of the investigated area consists of Mesozoic and Paleozoic sediments, while the areas near the shelf edge show a westward increasing wedge of Cenozoic deposits above the same sediments found to the east. Along the Norwegian coast and in the areas southwest of Bjornoya a rapid increase of sediments is noted, while a much more gentle westward growth is found in the main part of the Barents shelf. The data suggest the southern flank of Bjornoyrenna is an area of structural deformation. Structures that can be associated with salt diapirs are recorded in a limited area on Tromsoflaket." @default.
• W1981197993 created "2016-06-24" @default.
• W1981197993 creator A5061917634 @default.
• W1981197993 date "1974-07-01" @default.
• W1981197993 modified "2023-09-27" @default.
• W1981197993 title "Seismic refraction and reflection measurements in the southern Barents Sea" @default.
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• W1981197993 doi "https://doi.org/10.1016/0025-3227(74)90068-1" @default.
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