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dc.date.accessioned2023-02-20T16:06:42Z
dc.date.available2023-02-20T16:06:42Z
dc.date.created2022-05-22T18:10:34Z
dc.date.issued2022
dc.identifier.citationSlagstad, Trond Henderson, Lain Roberts, Nick MW Kulakov, Evgeniy Ganerød, Morgan Kirkland, Christopher L. Dalslåen, Bjørgunn Heggem Creaser, Robert A Coint, Nolwenn . Anorthosite formation and emplacement coupled with differential tectonic exhumation of ultrahigh-temperature rocks in a Sveconorwegian continental back-arc setting. Precambrian Research. 2022, 376
dc.identifier.urihttp://hdl.handle.net/10852/100173
dc.description.abstractThe tectonic setting and mechanisms and duration of emplacement of Proterozoic massif-type anorthosites and the significance of typically associated ultrahigh-temperature (UHT) host rocks have been debated for decades. This is particularly true of the Rogaland Anorthosite Province (RAP) in the SW Sveconorwegian Orogen. Earlier studies suggest that the RAP was emplaced over 1–3 Myr around 930 Ma towards the end of orogenesis, resulting in an up to 15–20 km-wide contact metamorphic aureole. However, our structural observations show that the RAP is located in the footwall of a 15 km-wide extensional detachment (Rogaland Extensional Detachment, RED), separating the intrusions and their UHT host rocks from weakly metamorphosed rocks in the hanging wall. U–Pb zircon dating of leucosome in extensional pull-aparts associated with the RED yields ages of 950–935 Ma, consistent with Re–Os molybdenite ages from brittle extensional structures in the hanging-wall block that range between 980 and 930 Ma. A metapelite in the immediate vicinity of the RAP yields a 950 Ma U–Pb age of matrix-hosted monazite, and part of the RAP was intruded by the Storgangen norite dike at ca. 950 Ma, providing a minimum age of emplacement. These ages are consistent with Ar–Ar hornblende and biotite ages that show rapid cooling of the footwall before 930 Ma, but slow cooling of the hanging wall. Field and geochronologic data suggest that the RAP formed and was emplaced over a long period of time, up to 100 Myr, with different emplacement mechanisms reflecting an evolving regional stress regime. The distribution of UHT rocks around the RAP reflects differential extensional exhumation between 980 and 930 Ma, not contact metamorphism. The duration and style of orogenic activity and externally (as opposed to gravitationally) driven extension suggest that the RAP formed in a continental back-arc setting.
dc.languageEN
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleAnorthosite formation and emplacement coupled with differential tectonic exhumation of ultrahigh-temperature rocks in a Sveconorwegian continental back-arc setting
dc.title.alternativeENEngelskEnglishAnorthosite formation and emplacement coupled with differential tectonic exhumation of ultrahigh-temperature rocks in a Sveconorwegian continental back-arc setting
dc.typeJournal article
dc.creator.authorSlagstad, Trond
dc.creator.authorHenderson, Lain
dc.creator.authorRoberts, Nick MW
dc.creator.authorKulakov, Evgeniy
dc.creator.authorGanerød, Morgan
dc.creator.authorKirkland, Christopher L.
dc.creator.authorDalslåen, Bjørgunn Heggem
dc.creator.authorCreaser, Robert A
dc.creator.authorCoint, Nolwenn
cristin.unitcode185,15,22,40
cristin.unitnameSenter for Jordens utvikling og dynamikk
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.cristin2026260
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Precambrian Research&rft.volume=376&rft.spage=&rft.date=2022
dc.identifier.jtitlePrecambrian Research
dc.identifier.volume376
dc.identifier.pagecount20
dc.identifier.doihttps://doi.org/10.1016/j.precamres.2022.106695
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn0301-9268
dc.type.versionPublishedVersion
cristin.articleid106695


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Attribution 4.0 International
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