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Kinematic retro-modelling of a cross-section through a thrust-and-fold belt: the Western Irish Namurian Basin

David C. Tanner, Frithjof A. Bense and Gabriele Ertl
Geological Society, London, Special Publications, 349, 61-76, 1 January 2011, https://doi.org/10.1144/SP349.4
David C. Tanner
1Geoscience Centre, University of GöttingenDepartment of Structural Geology and Geodynamics, Goldschmidtstr. 3, D-37077 Göttingen,Germany
2Present address: Leibniz Institute for Applied GeophysicsStilleweg 2, D-30655 Hannover,Germany
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Frithjof A. Bense
1Geoscience Centre, University of GöttingenDepartment of Structural Geology and Geodynamics, Goldschmidtstr. 3, D-37077 Göttingen,Germany
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Gabriele Ertl
1Geoscience Centre, University of GöttingenDepartment of Structural Geology and Geodynamics, Goldschmidtstr. 3, D-37077 Göttingen,Germany
3Present address: Lower Saxony State Authority for Mining, Energy and GeologyStilleweg 2, D-30655 Hannover,Germany
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Abstract

The Western Irish Namurian Basin (WINB) developed into a fold-and-thrust belt at the front of the northward-propagating Variscan orogenic wedge. Part of this basin is well exposed along the coast of County Clare, Ireland. From a detailed study that used an integrated GPS mapping approach, we produced a c. 50 km long, balanced cross-section, parallel to the tectonic transport vector. We sequentially decompacted and retro-deformed the Namurian strata in 7 stages to evaluate the palinspastic situation of the basin and the amount of shortening. By using passive markers in the model and a highly-detailed timescale, we were able to determine that shortening of the WINB, from the onset of Central Clare Group sedimentation was 7.44% (or 4.07 km) of which shortening due to folding accounts for c. 2.64% (c. 1.37 km), and therefore c. 4.80% (c. 2.69 km) was solely because of thrusting. The rate of horizontal shortening ranges from 1–34 mm a−1; this is within typical orogenic values.

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Geological Society, London, Special Publications: 349 (1)
Geological Society, London, Special Publications
Volume 349
2011
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Kinematic retro-modelling of a cross-section through a thrust-and-fold belt: the Western Irish Namurian Basin

David C. Tanner, Frithjof A. Bense and Gabriele Ertl
Geological Society, London, Special Publications, 349, 61-76, 1 January 2011, https://doi.org/10.1144/SP349.4
David C. Tanner
1Geoscience Centre, University of GöttingenDepartment of Structural Geology and Geodynamics, Goldschmidtstr. 3, D-37077 Göttingen,Germany
2Present address: Leibniz Institute for Applied GeophysicsStilleweg 2, D-30655 Hannover,Germany
  • Find this author on Google Scholar
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  • For correspondence: [email protected]
Frithjof A. Bense
1Geoscience Centre, University of GöttingenDepartment of Structural Geology and Geodynamics, Goldschmidtstr. 3, D-37077 Göttingen,Germany
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
Gabriele Ertl
1Geoscience Centre, University of GöttingenDepartment of Structural Geology and Geodynamics, Goldschmidtstr. 3, D-37077 Göttingen,Germany
3Present address: Lower Saxony State Authority for Mining, Energy and GeologyStilleweg 2, D-30655 Hannover,Germany
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  • Find this author on PubMed
  • Search for this author on this site

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Kinematic retro-modelling of a cross-section through a thrust-and-fold belt: the Western Irish Namurian Basin

David C. Tanner, Frithjof A. Bense and Gabriele Ertl
Geological Society, London, Special Publications, 349, 61-76, 1 January 2011, https://doi.org/10.1144/SP349.4
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