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dc.contributor.authorWiest, Johannes
dc.contributor.authorWrona, Thilo
dc.contributor.authorBauck, Marit Stokke
dc.contributor.authorFossen, Haakon
dc.contributor.authorGawthorpe, Rob
dc.contributor.authorOsmundsen, Per Terje
dc.contributor.authorFaleide, Jan Inge
dc.date.accessioned2020-11-17T07:36:40Z
dc.date.available2020-11-17T07:36:40Z
dc.date.created2020-11-08T17:52:17Z
dc.date.issued2020
dc.identifier.citationTectonics. 2020, 39:e2020TC006178 (10), 1-15.en_US
dc.identifier.issn0278-7407
dc.identifier.urihttps://hdl.handle.net/11250/2688124
dc.description.abstractExtensional systems evolve through different stages due to changes in the rheological state of the lithosphere. It is crucial to distinguish ductile structures formed before and during rifting, as both cases have important but contrasting bearings on the structural evolution. To address this issue, we present the illustrative ductile‐to‐brittle structural history of a metamorphic core complex (MCC) onshore and offshore western Norway. Combining geological field mapping with newly acquired 3‐D seismic reflection data, we correlate two distinct onshore basement units (BU1 and BU2) to corresponding offshore basement seismic facies (SF1 and SF2). Our interpretation reveals two 40 km wide domes (one onshore and one offshore), which both show characteristic kilometer‐scale, westward plunging upright folds. The gneiss domes fill antiformal culminations in the footwall of a >100 km long, shallowly west dipping, extensional detachment. Overlying Caledonian nappes and Devonian supradetachment basins occupy saddles of the hyperbolic detachment surface. Devonian collapse of the Caledonian orogen formed dome and detachment geometries. During North Sea rifting, brittle reactivation of the MCC resulted in complex fault patterns deviating from N‐S strike dominant at the eastern margin of the rift. Around 61°N, only minor N‐S faults (en_US
dc.language.isoengen_US
dc.publisherAmerican Geophysical Unionen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleFrom Caledonian collapse to North Sea Rift: The extended history of a metamorphic core complexen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber1-15en_US
dc.source.volume39:e2020TC006178en_US
dc.source.journalTectonicsen_US
dc.source.issue10en_US
dc.identifier.doi10.1029/2020TC006178
dc.identifier.cristin1845936
dc.description.localcode©2020. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. DOI: 10.1029/2020TC006178en_US
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cristin.fulltextoriginal
cristin.qualitycode2


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal