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TopoScandiaDeep Field Trip, Tectonic Topography of Norway's MTFC

dc.contributor.authorRedfield, T. F.
dc.contributor.authorNasuti, A.
dc.contributor.authorEbbing, J.
dc.contributor.authorStokke Bauck, M.
dc.contributor.authorGradmann, S.
dc.contributor.authorOsmundsen, P. T.
dc.date.accessioned2020-07-15T07:38:55Z
dc.date.available2020-07-15T07:38:55Z
dc.date.issued2011
dc.identifier.issn0800-3416
dc.identifier.urihttps://hdl.handle.net/11250/2664575
dc.description.abstractThis report describes a one-day field trip to observe relationships between brittle normal faults and landscape evolution on a post-glacial passive margin. The hypothesis that the great escarpment of western Norway was shaped after the main rift phases, through reactivation of inherited faults inboard of sharply tapering crystalline crust was based on combinations of apatite fission-track dating, structural geology, topographic analysis and interpretation of offshore deep seismic and potential field data. Comprised by nine stops, the trip begins in Molde and ends in Trondheim. The total driving time is a little over five hours.
dc.language.isoeng
dc.relation.ispartofseriesNGU-Rapport (2011.033)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectKONTINENTALSOKKEL
dc.subjectBERGGRUNNSGEOLOGI
dc.subjectFORKASTNING
dc.subjectLANDHEVNING
dc.subjectNEOTEKTONIKK
dc.subjectSKRED
dc.titleTopoScandiaDeep Field Trip, Tectonic Topography of Norway's MTFC
dc.typeReport
dc.description.localcode58005
dc.source.pagenumber47
dc.relation.project(327700) TopoScandia: Deep processes


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