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dc.contributor.advisorMartens, Iver
dc.contributor.advisorRydningen, Tom Arne
dc.contributor.authorHetland, Asbjørn
dc.date.accessioned2018-05-31T12:06:02Z
dc.date.available2018-05-31T12:06:02Z
dc.date.issued2018-05-15
dc.description.abstractWhile most established plays in the Barents Sea have occurred in the Mesozoic, the Alta and Gohta discoveries prove a new carbonate play concept, with a source rock that does not stem from the Jurassic. Based on depositional environment and TOC values from the Palaeozoic interval a source rock with Top Ørn as its bottom and Top Røye as its top was interpreted. Basin modelling carried out on this potential source rock concludes that the Palaeozoic interval in the Loppa High area have a good source potential. A total of 30 different models have been carried out and three highlighted models, the P10, P50 and P90 model all shows evidence of good maturity ranges (ranging from 0.5 %Ro to 1.5 %Ro) and generation potential.en_US
dc.identifier.urihttp://hdl.handle.net/10037/12814
dc.language.isoengen_US
dc.publisherUiT Norges arktiske universiteten_US
dc.publisherUiT The Arctic University of Norwayen_US
dc.rights.accessRightsopenAccessen_US
dc.subject.courseIDGEO-3900
dc.subjectVDP::Mathematics and natural science: 400::Geosciences: 450::Petroleum geology and petroleum geophysics: 464en_US
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Petroleumsgeologi og -geofysikk: 464en_US
dc.titleUse of 2D-seismic data and available wells to investigate the source potential of the Palaeozoic interval in the Loppa High area, SW Barents Seaen_US
dc.typeMaster thesisen_US
dc.typeMastergradsoppgaveen_US


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