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dc.contributor.advisorStefan, Buenz
dc.contributor.advisorJurgen, Mienert
dc.contributor.authorNjone, Isaac
dc.date.accessioned2014-12-11T08:57:49Z
dc.date.available2014-12-11T08:57:49Z
dc.date.issued2014-11-21
dc.description.abstractThe 3D seismic enable a better understanding of phreatomagmatic activity that occurred at the Gjallar ridge in the Vøring basin, mid-Norway. Structures associated with this activity were imaged and a causality relationship was established. Those structures included hydrothermal vent complexes, sill complexes and faults. The Kai formation significantly affected by polygonal faulting that were likely to play as evacuation structures for the fluid migrating to the BPU.en
dc.identifier.urihttps://hdl.handle.net/10037/6914
dc.identifier.urnURN:NBN:no-uit_munin_6517
dc.language.isoengen
dc.publisherUiT Norges arktiske universiteten
dc.publisherUiT The Arctic University of Norwayen
dc.rights.accessRightsopenAccess
dc.rights.holderCopyright 2014 The Author(s)
dc.rights.urihttps://creativecommons.org/licenses/by-nc-sa/3.0en_US
dc.rightsAttribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0)en_US
dc.subject.courseIDGEO-3900en
dc.subjectVDP::Technology: 500::Rock and petroleum disciplines: 510::Other rock and petroleum disciplines: 519en
dc.subjectVDP::Teknologi: 500::Berg? og petroleumsfag: 510::Andre berg? og petroleumsfagg: 519en
dc.titleHydrothermal Vent Activities At the Gjallar Ridge in the Vøring Basin, mid-Norwayen
dc.typeMaster thesisen
dc.typeMastergradsoppgaveen


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Attribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0)
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0)