dc.date.accessioned | 2023-09-29T15:13:42Z | |
dc.date.available | 2023-09-29T15:13:42Z | |
dc.date.created | 2023-04-25T10:27:08Z | |
dc.date.issued | 2023 | |
dc.identifier.citation | Grenne, Tor Gasser, Deta Bøe, Reidulv Corfu, Fernando Skår, Øyvind Slagstad, Trond . Mid-Ordovician stratigraphy and volcanism in the Hølonda area, Scandinavian Caledonides: complex tectonomagmatic development following arc–continent collision near the Laurentian margin of Iapetus. Journal of the Geological Society. 2023, 180(3) | |
dc.identifier.uri | http://hdl.handle.net/10852/105376 | |
dc.description.abstract | The Hølonda area of the central Scandinavian Caledonides is a key for models of the Caledonian orogen owing to its Ordovician fauna of Laurentian affinity, now stranded on the Baltic side during opening of the North Atlantic. Here, we present a revised stratigraphic and tectonomagmatic model based on remapping, sedimentology, igneous geochemistry, Nd and Sr isotopes and geochronology. The Hølonda Group (c. 470–461 Ma) reflects a transition from subaerial and shallow-marine deposition on a continental shelf to deeper-water sedimentation along a subsiding slope. Adakitic and mid-ocean ridge basalt type magmatism at c. 468 Ma was succeeded by benmoreitic–rhyolitic, shoshonitic, calc-alkaline and ultra-alkaline volcanism at c. 467–465 Ma. The complex magmatism followed arc–continent collision along a microcontinent outboard of Laurentia, associated with subduction polarity flip and slab rollback. This led to rifting and opening of a wide basin and its adjoining shelf on thickened orogenic lithosphere. Associated mantle upwelling and partial melting of depleted and variably metasomatized mantle occurred in a tectonomagmatic setting comparable with that of the central Mediterranean. The Hølonda–Ilfjellet setting is unique along the Caledonian–Appalachian orogen, possibly reflecting interaction with Laurentia-derived continental terranes at the northeastern end of the Taconian–Grampian orogenic tract. | |
dc.language | EN | |
dc.rights | Attribution 4.0 International | |
dc.rights.uri | https://creativecommons.org/licenses/by/4.0/ | |
dc.title | Mid-Ordovician stratigraphy and volcanism in the Hølonda area, Scandinavian Caledonides: complex tectonomagmatic development following arc–continent collision near the Laurentian margin of Iapetus | |
dc.title.alternative | ENEngelskEnglishMid-Ordovician stratigraphy and volcanism in the Hølonda area, Scandinavian Caledonides: complex tectonomagmatic development following arc–continent collision near the Laurentian margin of Iapetus | |
dc.type | Journal article | |
dc.creator.author | Grenne, Tor | |
dc.creator.author | Gasser, Deta | |
dc.creator.author | Bøe, Reidulv | |
dc.creator.author | Corfu, Fernando | |
dc.creator.author | Skår, Øyvind | |
dc.creator.author | Slagstad, Trond | |
cristin.unitcode | 185,15,22,0 | |
cristin.unitname | Institutt for geofag | |
cristin.ispublished | true | |
cristin.fulltext | original | |
cristin.qualitycode | 1 | |
dc.identifier.cristin | 2143129 | |
dc.identifier.bibliographiccitation | info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal of the Geological Society&rft.volume=180&rft.spage=&rft.date=2023 | |
dc.identifier.jtitle | Journal of the Geological Society | |
dc.identifier.volume | 180 | |
dc.identifier.issue | 3 | |
dc.identifier.pagecount | 22 | |
dc.identifier.doi | https://doi.org/10.1144/jgs2022-133 | |
dc.type.document | Tidsskriftartikkel | |
dc.type.peerreviewed | Peer reviewed | |
dc.source.issn | 0016-7649 | |
dc.type.version | PublishedVersion | |
cristin.articleid | jgs2022-133 | |