Potential mechanisms for the genesis of Cenozoic domal structures on the NE Atlantic margin: pros, cons and some new ideas
Abstract: The mild compressional structures of Cenozoic age on the passive margins bordering Norway, the UK, the Faroes and Ireland have been the subject of much discussion in the literature. Nevertheless, their origin remains enigmatic. Candidate mechanisms must be able to explain the generation of...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.552.1737 2023-05-15T16:11:16+02:00 Potential mechanisms for the genesis of Cenozoic domal structures on the NE Atlantic margin: pros, cons and some new ideas A. G. Doré E. R. Lundin N. J. Kusznir C. Pascal The Pennsylvania State University CiteSeerX Archives 2008 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.552.1737 http://www.mantleplumes.org/WebDocuments/Dore2008.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.552.1737 http://www.mantleplumes.org/WebDocuments/Dore2008.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.mantleplumes.org/WebDocuments/Dore2008.pdf text 2008 ftciteseerx 2016-01-08T11:36:31Z Abstract: The mild compressional structures of Cenozoic age on the passive margins bordering Norway, the UK, the Faroes and Ireland have been the subject of much discussion in the literature. Nevertheless, their origin remains enigmatic. Candidate mechanisms must be able to explain the generation of sufficient stress to cause deformation, the episodic nature of the structures and why they developed where they did. We examine these mechanisms and conclude that multiple causes are probable, while favouring body force as potentially the most important agent. The geometry and setting of the structures are incompatible with gravitational sliding and toe-thrusting, probably the commonest ‘compressive ’ structuring around the Atlantic margins. A passive mode of origin featuring drape or flank sedimentary loading probably emphasized some of the structures, but cannot be invoked as a primary mechanism. Likewise, reactivation of base-ment structure probably focused deformation but did not initiate it. Far-field orogenic stress from Alpine orogenic phases and from the West Spitsbergen–Eurekan folding and thrusting is also examined. This mechanism is attractive because of its potential to explain episodicity of the com-pressional structures. However, difficulties exist with stress transmission pathways from these fold belts, and the passive margin structures developed for much of their existence in the absence of Text Faroes Spitsbergen Unknown Norway |
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description |
Abstract: The mild compressional structures of Cenozoic age on the passive margins bordering Norway, the UK, the Faroes and Ireland have been the subject of much discussion in the literature. Nevertheless, their origin remains enigmatic. Candidate mechanisms must be able to explain the generation of sufficient stress to cause deformation, the episodic nature of the structures and why they developed where they did. We examine these mechanisms and conclude that multiple causes are probable, while favouring body force as potentially the most important agent. The geometry and setting of the structures are incompatible with gravitational sliding and toe-thrusting, probably the commonest ‘compressive ’ structuring around the Atlantic margins. A passive mode of origin featuring drape or flank sedimentary loading probably emphasized some of the structures, but cannot be invoked as a primary mechanism. Likewise, reactivation of base-ment structure probably focused deformation but did not initiate it. Far-field orogenic stress from Alpine orogenic phases and from the West Spitsbergen–Eurekan folding and thrusting is also examined. This mechanism is attractive because of its potential to explain episodicity of the com-pressional structures. However, difficulties exist with stress transmission pathways from these fold belts, and the passive margin structures developed for much of their existence in the absence of |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
A. G. Doré E. R. Lundin N. J. Kusznir C. Pascal |
spellingShingle |
A. G. Doré E. R. Lundin N. J. Kusznir C. Pascal Potential mechanisms for the genesis of Cenozoic domal structures on the NE Atlantic margin: pros, cons and some new ideas |
author_facet |
A. G. Doré E. R. Lundin N. J. Kusznir C. Pascal |
author_sort |
A. G. Doré |
title |
Potential mechanisms for the genesis of Cenozoic domal structures on the NE Atlantic margin: pros, cons and some new ideas |
title_short |
Potential mechanisms for the genesis of Cenozoic domal structures on the NE Atlantic margin: pros, cons and some new ideas |
title_full |
Potential mechanisms for the genesis of Cenozoic domal structures on the NE Atlantic margin: pros, cons and some new ideas |
title_fullStr |
Potential mechanisms for the genesis of Cenozoic domal structures on the NE Atlantic margin: pros, cons and some new ideas |
title_full_unstemmed |
Potential mechanisms for the genesis of Cenozoic domal structures on the NE Atlantic margin: pros, cons and some new ideas |
title_sort |
potential mechanisms for the genesis of cenozoic domal structures on the ne atlantic margin: pros, cons and some new ideas |
publishDate |
2008 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.552.1737 http://www.mantleplumes.org/WebDocuments/Dore2008.pdf |
geographic |
Norway |
geographic_facet |
Norway |
genre |
Faroes Spitsbergen |
genre_facet |
Faroes Spitsbergen |
op_source |
http://www.mantleplumes.org/WebDocuments/Dore2008.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.552.1737 http://www.mantleplumes.org/WebDocuments/Dore2008.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1765996408391860224 |