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dc.contributor.authorStoker, Martyn S.
dc.contributor.authorStewart, Margaret A.
dc.contributor.authorShannon, Patrick M.
dc.contributor.authorBjerager, Morten
dc.contributor.authorNielsen, Tove
dc.contributor.authorBlischke, Anett
dc.contributor.authorHjelstuen, Berit Oline Blihovde
dc.contributor.authorGaina, Carmen
dc.contributor.authorMcdermott, Kenneth G.
dc.contributor.authorÓlavsdóttir, Jana
dc.date.accessioned2018-09-04T13:28:03Z
dc.date.available2018-09-04T13:28:03Z
dc.date.issued2017
dc.PublishedStoker MS, Stewart, Shannon, Bjerager, Nielsen T, Blischke A, Hjelstuen BOB, Gaina C, Mcdermott, Ólavsdóttir. An overview of the Upper Palaeozoic-Mesozoic stratigraphy of the NE Atlantic region. Geological Society Special Publication. 2017;447(1):11-68eng
dc.identifier.issn0305-8719en_US
dc.identifier.issn2041-4927en_US
dc.identifier.urihttps://hdl.handle.net/1956/18371
dc.description.abstractThis study describes the distribution and stratigraphic range of the Upper Palaeozoic–Mesozoic succession in the NE Atlantic region, and is correlated between conjugate margins and along the axis of the NE Atlantic rift system. The stratigraphic framework has yielded important new constraints on the timing and nature of sedimentary basin development in the NE Atlantic, with implications for rifting and the break-up of the Pangaean supercontinent. From a regional perspective, the Permian–Triassic succession records a northwards transition from an arid interior to a passively subsiding, mixed carbonate–siliciclastic shelf margin. A Late Permian–earliest Triassic rift pulse has regional expression in the stratigraphic record. A fragmentary paralic to shallow-marine Lower Jurassic succession reflects Early Jurassic thermal subsidence and mild extensional tectonism; this was interrupted by widespread Mid-Jurassic uplift and erosion, and followed by an intense phase of Late Jurassic rifting in some (but not all) parts of the NE Atlantic region. The Cretaceous succession is dominated by thick basinal-marine deposits, which accumulated within and along a broad zone of extension and subsidence between Rockall and NE Greenland. There is no evidence for a substantive and continuous rift system along the proto-NE Atlantic until the Late Cretaceous.en_US
dc.language.isoengeng
dc.publisherThe Geological Society of Londonen_US
dc.rightsAttribution CC BYeng
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/eng
dc.titleAn overview of the Upper Palaeozoic-Mesozoic stratigraphy of the NE Atlantic regionen_US
dc.typePeer reviewed
dc.typeJournal article
dc.date.updated2018-02-15T09:57:32Z
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2017 The Author(s)en_US
dc.identifier.doihttps://doi.org/10.1144/sp447.2
dc.identifier.cristin1564093
dc.source.journalGeological Society Special Publication


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