Constraining the tectonic evolution of rifted continental margins by U–Pb calcite dating

Abstract We employ U–Pb calcite dating of structurally-controlled fracture fills within crystalline Caledonian basement in western Norway to reveal subtle large-scale tectonic events that affected this rifted continental margin. The ages (15 in total) fall into four distinct groups with ages mainly...

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Published in:Scientific Reports
Main Authors: Åse Hestnes, Kerstin Drost, Tor O. Sømme, Deta Gasser, Thomas Scheiber, Henriette Linge, David Chew, Joachim Jacobs
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
R
Q
Online Access:https://doi.org/10.1038/s41598-023-34649-z
https://doaj.org/article/88f1bd68f8414d65877680ebe13fb8c7
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spelling ftdoajarticles:oai:doaj.org/article:88f1bd68f8414d65877680ebe13fb8c7 2023-06-11T04:13:11+02:00 Constraining the tectonic evolution of rifted continental margins by U–Pb calcite dating Åse Hestnes Kerstin Drost Tor O. Sømme Deta Gasser Thomas Scheiber Henriette Linge David Chew Joachim Jacobs 2023-05-01T00:00:00Z https://doi.org/10.1038/s41598-023-34649-z https://doaj.org/article/88f1bd68f8414d65877680ebe13fb8c7 EN eng Nature Portfolio https://doi.org/10.1038/s41598-023-34649-z https://doaj.org/toc/2045-2322 doi:10.1038/s41598-023-34649-z 2045-2322 https://doaj.org/article/88f1bd68f8414d65877680ebe13fb8c7 Scientific Reports, Vol 13, Iss 1, Pp 1-9 (2023) Medicine R Science Q article 2023 ftdoajarticles https://doi.org/10.1038/s41598-023-34649-z 2023-05-28T00:38:06Z Abstract We employ U–Pb calcite dating of structurally-controlled fracture fills within crystalline Caledonian basement in western Norway to reveal subtle large-scale tectonic events that affected this rifted continental margin. The ages (15 in total) fall into four distinct groups with ages mainly ranging from latest Cretaceous to Pleistocene. (1) The three oldest (Triassic-Jurassic) ages refine the complex faulting history of a reactivated fault strand originated from the Caledonian collapse and broadly correlate with known rifting events offshore. (2) Two ages of ca. 90–80 Ma relate to lithospheric stretching and normal fault reactivation of a major ENE-WSW trending late Caledonian shear zone. (3) We correlate five ages between ca. 70 and 60 Ma with far-field effects and dynamic uplift related to the proto-Iceland mantle plume, the effect and extent of which is highly debated. (4) The five youngest ages (< 50 Ma) from distinct NE–SW trending faults are interpreted to represent several episodes of post-breakup fracture dilation, indicating a long-lived Cenozoic deformation history. Our new U–Pb data combined with structural and isotopic data show that much larger tracts of the uplifted continental margin of western Norway have been affected by far-field tectonic stresses than previously anticipated, with deformation continuing into the late Cenozoic. Article in Journal/Newspaper Iceland Directory of Open Access Journals: DOAJ Articles Norway Scientific Reports 13 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Åse Hestnes
Kerstin Drost
Tor O. Sømme
Deta Gasser
Thomas Scheiber
Henriette Linge
David Chew
Joachim Jacobs
Constraining the tectonic evolution of rifted continental margins by U–Pb calcite dating
topic_facet Medicine
R
Science
Q
description Abstract We employ U–Pb calcite dating of structurally-controlled fracture fills within crystalline Caledonian basement in western Norway to reveal subtle large-scale tectonic events that affected this rifted continental margin. The ages (15 in total) fall into four distinct groups with ages mainly ranging from latest Cretaceous to Pleistocene. (1) The three oldest (Triassic-Jurassic) ages refine the complex faulting history of a reactivated fault strand originated from the Caledonian collapse and broadly correlate with known rifting events offshore. (2) Two ages of ca. 90–80 Ma relate to lithospheric stretching and normal fault reactivation of a major ENE-WSW trending late Caledonian shear zone. (3) We correlate five ages between ca. 70 and 60 Ma with far-field effects and dynamic uplift related to the proto-Iceland mantle plume, the effect and extent of which is highly debated. (4) The five youngest ages (< 50 Ma) from distinct NE–SW trending faults are interpreted to represent several episodes of post-breakup fracture dilation, indicating a long-lived Cenozoic deformation history. Our new U–Pb data combined with structural and isotopic data show that much larger tracts of the uplifted continental margin of western Norway have been affected by far-field tectonic stresses than previously anticipated, with deformation continuing into the late Cenozoic.
format Article in Journal/Newspaper
author Åse Hestnes
Kerstin Drost
Tor O. Sømme
Deta Gasser
Thomas Scheiber
Henriette Linge
David Chew
Joachim Jacobs
author_facet Åse Hestnes
Kerstin Drost
Tor O. Sømme
Deta Gasser
Thomas Scheiber
Henriette Linge
David Chew
Joachim Jacobs
author_sort Åse Hestnes
title Constraining the tectonic evolution of rifted continental margins by U–Pb calcite dating
title_short Constraining the tectonic evolution of rifted continental margins by U–Pb calcite dating
title_full Constraining the tectonic evolution of rifted continental margins by U–Pb calcite dating
title_fullStr Constraining the tectonic evolution of rifted continental margins by U–Pb calcite dating
title_full_unstemmed Constraining the tectonic evolution of rifted continental margins by U–Pb calcite dating
title_sort constraining the tectonic evolution of rifted continental margins by u–pb calcite dating
publisher Nature Portfolio
publishDate 2023
url https://doi.org/10.1038/s41598-023-34649-z
https://doaj.org/article/88f1bd68f8414d65877680ebe13fb8c7
geographic Norway
geographic_facet Norway
genre Iceland
genre_facet Iceland
op_source Scientific Reports, Vol 13, Iss 1, Pp 1-9 (2023)
op_relation https://doi.org/10.1038/s41598-023-34649-z
https://doaj.org/toc/2045-2322
doi:10.1038/s41598-023-34649-z
2045-2322
https://doaj.org/article/88f1bd68f8414d65877680ebe13fb8c7
op_doi https://doi.org/10.1038/s41598-023-34649-z
container_title Scientific Reports
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