A. Bubeck
Extension parallel to the rift zone during segmented fault growth: application to the evolution of the NE Atlantic
Bubeck, A.; Walker, R.J.; Imber, J.; Holdsworth, R.E.; MacLeod, C.J.; Holwell, D.A.
Authors
R.J. Walker
J. Imber
Professor Bob Holdsworth r.e.holdsworth@durham.ac.uk
Professor
C.J. MacLeod
D.A. Holwell
Abstract
The mechanical interaction of propagating normal faults is known to influence the linkage geometry of first-order faults, and the development of second-order faults and fractures, which transfer displacement within relay zones. Here we use natural examples of growth faults from two active volcanic rift zones (Koa`e, island of Hawai`i, and Krafla, northern Iceland) to illustrate the importance of horizontal-plane extension (heave) gradients, and associated vertical axis rotations, in evolving continental rift systems. Second-order extension and extensional-shear faults within the relay zones variably resolve components of regional extension, and components of extension and/or shortening parallel to the rift zone, to accommodate the inherently three-dimensional (3-D) strains associated with relay zone development and rotation. Such a configuration involves volume increase, which is accommodated at the surface by open fractures; in the subsurface this may be accommodated by veins or dikes oriented obliquely and normal to the rift axis. To consider the scalability of the effects of relay zone rotations, we compare the geometry and kinematics of fault and fracture sets in the Koa`e and Krafla rift zones with data from exhumed contemporaneous fault and dike systems developed within a > 5×104 km2 relay system that developed during formation of the NE Atlantic margins. Based on the findings presented here we propose a new conceptual model for the evolution of segmented continental rift basins on the NE Atlantic margins.
Citation
Bubeck, A., Walker, R., Imber, J., Holdsworth, R., MacLeod, C., & Holwell, D. (2017). Extension parallel to the rift zone during segmented fault growth: application to the evolution of the NE Atlantic. Solid Earth, 8(6), 1161-1180. https://doi.org/10.5194/se-8-1161-2017
Journal Article Type | Article |
---|---|
Acceptance Date | Oct 17, 2017 |
Online Publication Date | Nov 22, 2017 |
Publication Date | Nov 22, 2017 |
Deposit Date | Oct 18, 2017 |
Publicly Available Date | Oct 18, 2017 |
Journal | Solid Earth and Discussions |
Print ISSN | 1869-9510 |
Electronic ISSN | 1869-9529 |
Publisher | European Geosciences Union |
Peer Reviewed | Peer Reviewed |
Volume | 8 |
Issue | 6 |
Pages | 1161-1180 |
DOI | https://doi.org/10.5194/se-8-1161-2017 |
Public URL | https://durham-repository.worktribe.com/output/1346232 |
Files
Published Journal Article
(19.8 Mb)
PDF
Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/
Accepted Journal Article
(6.7 Mb)
PDF
Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/
Copyright Statement
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
You might also like
The Humbly Grove, Herriard and Hester’s Copse Fields, UK onshore
(2020)
Journal Article
Downloadable Citations
About Durham Research Online (DRO)
Administrator e-mail: dro.admin@durham.ac.uk
This application uses the following open-source libraries:
SheetJS Community Edition
Apache License Version 2.0 (http://www.apache.org/licenses/)
PDF.js
Apache License Version 2.0 (http://www.apache.org/licenses/)
Font Awesome
SIL OFL 1.1 (http://scripts.sil.org/OFL)
MIT License (http://opensource.org/licenses/mit-license.html)
CC BY 3.0 ( http://creativecommons.org/licenses/by/3.0/)
Powered by Worktribe © 2024
Advanced Search