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Regional-scale lateral variation and linkage in ductile thrust architecture: the Oykel Transverse Zone, and mullions, in the Moine Nappe, NW Scotland

A. G. Leslie, M. Krabbendam, G. S. Kimbell and R. A. Strachan
Geological Society, London, Special Publications, 335, 359-381, 1 January 2010, https://doi.org/10.1144/SP335.17
A. G. Leslie
1British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, UK
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M. Krabbendam
1British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, UK
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G. S. Kimbell
2British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottingham NG12 5GG, UK
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R. A. Strachan
3School of Earth & Environmental Sciences, University of Portsmouth, Burnaby Road, Portsmouth PO1 3QL, UK
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Abstract

Sharp lateral changes in structural geometry of ductile thrust stacks are not widely reported. A regional-scale lateral culmination wall forms the southern boundary of the Cassley Culmination in Moine rocks in the Caledonides of Sutherland, Northern Scotland. This culmination wall is part of the Oykel Transverse Zone (OTZ), a kilometre-scale shear zone characterized by constrictional finite strain fabrics aligned sub-parallel to the regional WNW-directed thrust transport direction. Main phase folds and fabrics in the transverse zone hanging wall are folded by main phase folds and fabrics in the footwall, thus recording foreland-propagating ductile deformation. South of the Cassley Culmination, shortening occurred uniformly, without development of discrete subsidiary thrusts; distributed deformation (fold development) alternated with localized thrusting within the culmination. The classic ESE-plunging mullions at Oykel Bridge are an integral part of the OTZ and were generated by constriction aligned sub-parallel to the transport direction. Constriction is attributed to differential, transtensional movement across the OTZ during culmination development. Subsequent formation of the underlying Assynt Culmination further accentuated upward-bulging of the Cassley Culmination, amplifying the lateral change across the transverse zone. The OTZ aligns with a pronounced gravity gradient on the south-western side of the Lairg gravity low. Interpretive modelling relates this gradient to a buried basement ramp that possibly controlled the location of the transverse zone.

  • © The Geological Society of London 2010
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Geological Society, London, Special Publications: 335 (1)
Geological Society, London, Special Publications
Volume 335
2010
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Regional-scale lateral variation and linkage in ductile thrust architecture: the Oykel Transverse Zone, and mullions, in the Moine Nappe, NW Scotland

A. G. Leslie, M. Krabbendam, G. S. Kimbell and R. A. Strachan
Geological Society, London, Special Publications, 335, 359-381, 1 January 2010, https://doi.org/10.1144/SP335.17
A. G. Leslie
1British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, UK
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
  • For correspondence: agle@bgs.ac.uk
M. Krabbendam
1British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, UK
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  • Find this author on PubMed
  • Search for this author on this site
G. S. Kimbell
2British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottingham NG12 5GG, UK
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R. A. Strachan
3School of Earth & Environmental Sciences, University of Portsmouth, Burnaby Road, Portsmouth PO1 3QL, UK
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  • Search for this author on this site

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Regional-scale lateral variation and linkage in ductile thrust architecture: the Oykel Transverse Zone, and mullions, in the Moine Nappe, NW Scotland

A. G. Leslie, M. Krabbendam, G. S. Kimbell and R. A. Strachan
Geological Society, London, Special Publications, 335, 359-381, 1 January 2010, https://doi.org/10.1144/SP335.17
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  • Article
    • Abstract
    • Geological setting
    • The Cassley Culmination: overview
    • Structure and lithologies of the Achness Nappe
    • Structure and lithologies of the Ben Hope Nappe
    • Structure and lithologies of the Moine Nappe (sensu stricto)
    • Relationship between fabric development and folding in different nappes
    • Termination of the Cassley Culmination
    • Geophysical data: the Lairg gravity low
    • Discussion
    • Conclusion
    • Acknowledgments
    • References
  • Figures & Data
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