Rift magmatism on the Eurasia basin margin: U-Pb baddeleyite ages of alkaline dyke swarms in North Greenland
(2015) In Journal of the Geological Society 172(6). p.721-726- Abstract
- The opening of the Arctic Ocean involved multiple stages of continental rifting and intrusion of extensive dyke swarms. To trace tectonomagmatic processes of the High Arctic, we present the first U-Pb ages for alkaline dyke swarms of North Greenland. Concordia ages of 80.8 +/- 0.6 and 82.1 +/- 1.5 Ma indicate that north-south and east-west dykes are coeval. The north-south dykes reflect initial east-west rifting that led to break-up along the Gakkel Ridge and formation of the Eurasia Basin. The east-west dykes reflect local variations in the stress field associated with reactivated Palaeozoic faults.
Please use this url to cite or link to this publication:
https://lup.lub.lu.se/record/8389411
- author
- Thorarinsson, Sigurjon B. ; Söderlund, Ulf LU ; Dossing, Arne ; Holm, Paul M. ; Ernst, Richard E. and Tegner, Christian
- organization
- publishing date
- 2015
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Journal of the Geological Society
- volume
- 172
- issue
- 6
- pages
- 721 - 726
- publisher
- Geological Society of London
- external identifiers
-
- wos:000363986900004
- scopus:84945914662
- ISSN
- 2041-479X
- DOI
- 10.1144/jgs2015-049
- language
- English
- LU publication?
- yes
- id
- 45e38f17-6238-4cc9-9567-f8b0b46a2d72 (old id 8389411)
- date added to LUP
- 2016-04-01 10:47:14
- date last changed
- 2022-03-04 22:46:04
@article{45e38f17-6238-4cc9-9567-f8b0b46a2d72, abstract = {{The opening of the Arctic Ocean involved multiple stages of continental rifting and intrusion of extensive dyke swarms. To trace tectonomagmatic processes of the High Arctic, we present the first U-Pb ages for alkaline dyke swarms of North Greenland. Concordia ages of 80.8 +/- 0.6 and 82.1 +/- 1.5 Ma indicate that north-south and east-west dykes are coeval. The north-south dykes reflect initial east-west rifting that led to break-up along the Gakkel Ridge and formation of the Eurasia Basin. The east-west dykes reflect local variations in the stress field associated with reactivated Palaeozoic faults.}}, author = {{Thorarinsson, Sigurjon B. and Söderlund, Ulf and Dossing, Arne and Holm, Paul M. and Ernst, Richard E. and Tegner, Christian}}, issn = {{2041-479X}}, language = {{eng}}, number = {{6}}, pages = {{721--726}}, publisher = {{Geological Society of London}}, series = {{Journal of the Geological Society}}, title = {{Rift magmatism on the Eurasia basin margin: U-Pb baddeleyite ages of alkaline dyke swarms in North Greenland}}, url = {{http://dx.doi.org/10.1144/jgs2015-049}}, doi = {{10.1144/jgs2015-049}}, volume = {{172}}, year = {{2015}}, }