Christian Schiffer
Structural inheritance in the North Atlantic
Schiffer, Christian; Doré, Anthony G.; Foulger, Gillian R.; Franke, Dieter; Geoffroy, Laurent; Gernigon, Laurent; Holdsworth, Robert; Kusznir, Nick; Lundin, Erik; McCaffrey, Ken; Peace, Alex; Petersen, Kenni D.; Phillips, Thomas; Stephenson, Randell; Stoker, Martyn S.; Welford, Kim
Authors
Anthony G. Doré
Gillian Foulger g.r.foulger@durham.ac.uk
Emeritus Professor
Dieter Franke
Laurent Geoffroy
Laurent Gernigon
Professor Bob Holdsworth r.e.holdsworth@durham.ac.uk
Professor
Nick Kusznir
Erik Lundin
Professor Kenneth Mccaffrey k.j.w.mccaffrey@durham.ac.uk
Head of Department
Alex Peace
Kenni D. Petersen
Thomas Phillips
Randell Stephenson
Martyn S. Stoker
Kim Welford
Abstract
The North Atlantic, extending from the Charlie Gibbs Fracture Zone to the north Norway-Greenland-Svalbard margins, is regarded as both a classic case of structural inheritance and an exemplar for the Wilson-cycle concept. This paper examines different aspects of structural inheritance in the Circum-North Atlantic region: 1) as a function of rejuvenation from lithospheric to crustal scales, and 2) in terms of sequential rifting and opening of the ocean and its margins, including a series of failed rift systems. We summarise and evaluate the role of fundamental lithospheric structures such as mantle fabric and composition, lower crustal inhomogeneities, orogenic belts, and major strike-slip faults during breakup. We relate these to the development and shaping of the NE Atlantic rifted margins, localisation of magmatism, and microcontinent release. We show that, although inheritance is common on multiple scales, the Wilson Cycle is at best an imperfect model for the Circum-North Atlantic region. Observations from the NE Atlantic suggest depth dependency in inheritance (surface, crust, mantle) with selective rejuvenation depending on time-scales, stress field orientations and thermal regime. Specifically, post-Caledonian reactivation to form the North Atlantic rift systems essentially followed pre-existing orogenic crustal structures, while eventual breakup reflected a change in stress field and exploitation of a deeper-seated, lithospheric-scale shear fabrics. We infer that, although collapse of an orogenic belt and eventual transition to a new ocean does occur, it is by no means inevitable.
Citation
Schiffer, C., Doré, A. G., Foulger, G. R., Franke, D., Geoffroy, L., Gernigon, L., Holdsworth, R., Kusznir, N., Lundin, E., McCaffrey, K., Peace, A., Petersen, K. D., Phillips, T., Stephenson, R., Stoker, M. S., & Welford, K. (2020). Structural inheritance in the North Atlantic. Earth-Science Reviews, 206, Article 102975. https://doi.org/10.1016/j.earscirev.2019.102975
Journal Article Type | Article |
---|---|
Acceptance Date | Oct 4, 2019 |
Online Publication Date | Oct 18, 2019 |
Publication Date | 2020-07 |
Deposit Date | Nov 4, 2019 |
Publicly Available Date | Oct 18, 2020 |
Journal | Earth-Science Reviews |
Print ISSN | 0012-8252 |
Publisher | Elsevier |
Peer Reviewed | Peer Reviewed |
Volume | 206 |
Article Number | 102975 |
DOI | https://doi.org/10.1016/j.earscirev.2019.102975 |
Public URL | https://durham-repository.worktribe.com/output/1284814 |
Files
Accepted Journal Article
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Publisher Licence URL
http://creativecommons.org/licenses/by-nc-nd/4.0/
Copyright Statement
© 2019 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/
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