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.
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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- 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
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Latest update: 08 Nov 2024
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...