Articles | Volume 9, issue 2
https://doi.org/10.5194/se-9-403-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-9-403-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Apr 2018
Research article |
| 09 Apr 2018
| 09 Apr 2018
Oblique reactivation of lithosphere-scale lineaments controls rift physiography – the upper-crustal expression of the Sorgenfrei–Tornquist Zone, offshore southern Norway
Basins Research Group (BRG), Department of Earth Science and
Engineering, Imperial College, South Kensington Campus, Prince Consort Road,
London, SW7 2BP, UK
Christopher A.-L. Jackson
Basins Research Group (BRG), Department of Earth Science and
Engineering, Imperial College, South Kensington Campus, Prince Consort Road,
London, SW7 2BP, UK
Rebecca E. Bell
Basins Research Group (BRG), Department of Earth Science and
Engineering, Imperial College, South Kensington Campus, Prince Consort Road,
London, SW7 2BP, UK
Oliver B. Duffy
Bureau of Economic Geology, Jackson School of Geosciences, The
University of Texas at Austin, University Station, Box X, Austin, TX
78713-8924, USA
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- Superposed fracture networks D. Peacock et al. 10.1017/S0016756823000730
- Evolution of slip partitioning in a major continental margin strike-slip fault system during a transition to oblique plate-margin tectonics: Insight into the evolution of the Garlock fault zone, California (USA) J. Andrew et al. 10.1130/GES02483.1
- Rivers, reefs and deltas: geomorphological evolution of the Jurassic of the Farsund Basin, offshore southern Norway T. Phillips et al. 10.1144/petgeo2018-056
- Analogue modelling of the inversion of multiple extensional basins in foreland fold-and-thrust belts N. Molnar & S. Buiter 10.5194/se-14-213-2023
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- Ridge Subduction as a Mechanism for Strike-Slip System Formation: Examples from the Chugach Metamorphic Complex, Alaska, and the Norumbega Fault System, Maine M. Scharman & B. Hooks 10.2139/ssrn.4127317
- Oblique rifting: the rule, not the exception S. Brune et al. 10.5194/se-9-1187-2018
- Early Cretaceous evolution of the Tromsø Basin, SW Barents Sea, Norway B. Kairanov et al. 10.1016/j.marpetgeo.2020.104714
- Magma-assisted fragmentation of Pangea: Continental breakup initiation and propagation H. Guan et al. 10.1016/j.gr.2021.04.003
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- Impact of sub-basalt thrust systems on the Faroe continental shelf for the late Paleoproterozoic–Cenozoic tectonic evolution of the margin. J. Koehl et al. 10.12688/openreseurope.18284.1
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- Evidence for Basement Reactivation during the Opening of the Labrador Sea from the Makkovik Province, Labrador, Canada: Insights from Field Data and Numerical Models A. Peace et al. 10.3390/geosciences8080308
- Geophysical Constraints on the Crustal Architecture of the Transtensional Warm Springs Valley Fault Zone, Northern Walker Lane, Western Nevada, USA R. Briggs et al. 10.1029/2020JB020757
- Scale matters: The influence of structural inheritance on fracture patterns A. Samsu et al. 10.1016/j.jsg.2019.103896
- Deformation driven by deep and distant structures: Influence of a mantle lithosphere suture in the Ouachita orogeny, southeastern United States P. Heron et al. 10.1130/G45690.1
- Control of inherited accreted lithospheric heterogeneity on the architecture and the low, long-term subsidence rate of intracratonic basins P. Perron et al. 10.1051/bsgf/2020038
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Latest update: 29 Jan 2025
Short summary
We use seismic reflection data and quantitative fault analyses to examine how a sub-crustal lineament, the Sorgenfrei–Tornquist Zone, is expressed within upper-crustal rift systems off the shore of southern Norway. We document repeated reactivation of upper-crustal faults, displaying both sinistral and dextral oblique activity, which we link to underlying lineament and regional tectonics. We show how sub-crustal lineaments influence rift evolution and offer insights into past tectonic events.
We use seismic reflection data and quantitative fault analyses to examine how a sub-crustal...
