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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36 citations as recorded by crossref.
- Impact of pre-existing fabrics and multi-phase oblique extension on Cenozoic fault patterns, Wichianburi sub-basin of the Phetchabun rift, Thailand S. Pongwapee et al. 10.1016/j.jsg.2018.11.012
- Pre-inversion normal fault geometry controls inversion style and magnitude, Farsund Basin, offshore southern Norway T. Phillips et al. 10.5194/se-11-1489-2020
- Influence of basement heterogeneity on the architecture of low subsidence rate Paleozoic intracratonic basins (Reggane, Ahnet, Mouydir and Illizi basins, Hoggar Massif) P. Perron et al. 10.5194/se-9-1239-2018
- The near-surface structure in the area of the Børglum fault, Sorgenfrei-Tornquist Zone, northern Denmark: Implications for fault kinematics, timing of fault activity and fault control on tunnel valley formation C. Brandes et al. 10.1016/j.quascirev.2022.107619
- Podolian, Saxonian and baltic plates – Teisseyre–Tornquist Line and the edge of the East European Craton M. Grad 10.1016/j.chemer.2019.03.002
- A review of Pangaea dispersal and Large Igneous Provinces – In search of a causative mechanism A. Peace et al. 10.1016/j.earscirev.2019.102902
- Repeated brittle reactivations of a pre-existing plastic shear zone: combined K–Ar and 40Ar–39Ar geochronology of the long-lived (>700 Ma) Himdalen–Ørje Deformation Zone, SE Norway E. Torgersen et al. 10.1017/S0016756822000966
- 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
- Paleozoic-Mesozoic tectono-sedimentary evolution and magmatism of the Egersund Basin area, Norwegian central North Sea M. Kalani et al. 10.1016/j.marpetgeo.2020.104642
- Application of Automated Throw Backstripping Method to Characterize Recent Faulting Activity Migration in the Al Hoceima Bay (Northeast Morocco): Geodynamic Implications V. Tendero-Salmerón et al. 10.3389/feart.2021.645942
- A reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–Triassic P. Angrand et al. 10.5194/se-11-1313-2020
- Influence of pre-existing faults on Cenozoic structures in the Chengbei sag and the Wuhaozhuang area, Bohai Bay Basin, East China D. Wang et al. 10.1016/j.marpetgeo.2022.105539
- 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
- Seismic amplitude and attribute data from Mesozoic strata in the Skagerrak (Danish-Norwegian North Sea): Indicators for fluid migration and seal bypass systems H. Grob et al. 10.1016/j.marpetgeo.2020.104596
- Segmentation of Rifts Through Structural Inheritance: Creation of the Davis Strait P. Heron et al. 10.1029/2019TC005578
- Terrane Boundary Reactivation, Barriers to Lateral Fault Propagation and Reactivated Fabrics: Rifting Across the Median Batholith Zone, Great South Basin, New Zealand T. Phillips & K. McCaffrey 10.1029/2019TC005772
- Rift-related magmatism on magma-poor margins: Structural and potential-field analyses of the Mesozoic Notre Dame Bay intrusions, Newfoundland, Canada and their link to North Atlantic Opening A. Peace et al. 10.1016/j.tecto.2018.07.025
- 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
- Structural inheritance and its control on overpressure preservation in mature sedimentary basins (Dongying depression, Bohai Bay Basin, China) Z. Tao et al. 10.1016/j.marpetgeo.2021.105504
- Strain partitioning dominated growth of strike-slip fault: Insight from the Tan-Lu fault in Eastern China R. Chu et al. 10.1016/j.jsg.2024.105126
- Tectonostratigraphic evolution of the Slyne Basin C. O'Sullivan et al. 10.5194/se-13-1649-2022
- Conjugate margins — An oversimplification of the complex southern North Atlantic rift and spreading system? A. Peace & J. Kim Welford 10.1190/INT-2019-0087.1
- Publisher’s Note 10.1016/j.earscirev.2019.05.009
- The orogenic bridge theory: towards a predictive tool for past and future plate tectonics J. Koehl & G. Foulger 10.12688/openreseurope.17238.1
- Conjugate volcanic passive margins in the austral segment of the South Atlantic – Architecture and development F. Chauvet et al. 10.1016/j.earscirev.2020.103461
- Halokinetically Overprinted Tectonic Inversion of the Penobscot 3D Volume Offshore Nova Scotia, Canada A. Peace et al. 10.1007/s00024-024-03462-8
Latest update: 23 Apr 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...
