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dc.contributor.advisorLaberg, Jan Sverre
dc.contributor.advisorRydningen, Tom Arne
dc.contributor.authorHøgseth, Gert Vidar
dc.date.accessioned2016-06-20T12:30:36Z
dc.date.available2016-06-20T12:30:36Z
dc.date.issued2016-05-15
dc.description.abstract2D seismic data have been analysed to study the Cenozoic pre-glacial sedimentary environment on the southwest Barents Sea margin and the Lofoten Basin. Based on a seismic stratigraphic analysis and correlation to previous work in the area, the pre-glacial seismic unit G0 has been subdivided into four. The four units have been described and discussed with regards to the geometry and internal seismic facies, and the sedimentary processes and depositional environment dominating during the deposition of the seismic units have been outlined.en_US
dc.identifier.urihttps://hdl.handle.net/10037/9321
dc.identifier.urnURN:NBN:no-uit_munin_8874
dc.language.isoengen_US
dc.publisherUiT Norges arktiske universiteten_US
dc.publisherUiT The Arctic University of Norwayen_US
dc.rights.accessRightsopenAccess
dc.subject.courseIDGEO-3900
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Marin geologi: 466en_US
dc.subjectVDP::Mathematics and natural science: 400::Geosciences: 450::Marine geology: 466en_US
dc.titleThe Cenozoic pre-glacial sedimentary environment of the SW Barents Sea continental margin – Lofoten Basinen_US
dc.typeMaster thesisen_US
dc.typeMastergradsoppgaveen_US


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