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Strike-slip influenced stratigraphic and structural development of the Foula Sandstone Group, Shetland: implications for offshore Devonian basin development on the northern UK continental shelf

Utley, T. A.G.; Holdsworth, R. E.; Blackbourn, G. A.; Dempsey, E.; Strachan, R. A.; McCaffrey, K. J.W.; Morton, A. C.; Bird, A. F.; Jones, R. R.; Saßnowski, A.; Walker, R. J.

Authors

T. A.G. Utley

R. E. Holdsworth

G. A. Blackbourn

Profile image of Eddie Dempsey

Dr Eddie Dempsey E.Dempsey@hull.ac.uk
Senior Lecturer in Structural Geology and Geohazards

R. A. Strachan

K. J.W. McCaffrey

A. C. Morton

R. R. Jones

A. Saßnowski

R. J. Walker



Abstract

The island of Foula, located 25 km SW of Shetland, preserves a gently folded, 1.6 km thick sequence of Middle Devonian sandstones spectacularly exposed in kilometre-long cliff sections >350 m high. These rocks unconformably overlie likely Precambrian-age amphibolite facies basement rocks that are intruded by sheeted granites. The onshore succession is similar in age to the nearby Lower Clair Group offshore to the west. New mapping, incorporating the use of drone imagery in the inaccessible cliff sections, uses down-plunge projections to show that growth folding and faulting on Foula were contemporaneous with sedimentation during basin filling. The large-scale structural geometry is consistent with the regional constrictional strain due to the sinistral transtension associated with movements along the Walls Boundary–Great Glen fault zone system during the Mid-Devonian. Detrital zircon provenance studies indicate that the Devonian sequences of Foula (and nearby Melby in western Shetland) show similarities with the Clair Group and Orkney successions. We suggest that NE–SW transtensional fold development contemporaneous with regional subsidence in the Devonian basins of Scotland may be more widespread than previously realized. Large, kilometre-scale folds previously interpreted to be related to Permo-Carboniferous inversion may therefore have initiated earlier in the basin evolution sequence than previously realized.

Citation

Utley, T. A., Holdsworth, R. E., Blackbourn, G. A., Dempsey, E., Strachan, R. A., McCaffrey, K. J., Morton, A. C., Bird, A. F., Jones, R. R., Saßnowski, A., & Walker, R. J. (2023). Strike-slip influenced stratigraphic and structural development of the Foula Sandstone Group, Shetland: implications for offshore Devonian basin development on the northern UK continental shelf. Journal of the Geological Society, 180(3), Article jgs2022-148. https://doi.org/10.1144/jgs2022-148

Journal Article Type Article
Acceptance Date Feb 17, 2023
Online Publication Date Feb 28, 2023
Publication Date May 5, 2023
Deposit Date Jul 18, 2023
Publicly Available Date Jul 21, 2023
Journal Journal of the Geological Society
Print ISSN 0016-7649
Publisher The Geological Society
Peer Reviewed Peer Reviewed
Volume 180
Issue 3
Article Number jgs2022-148
DOI https://doi.org/10.1144/jgs2022-148
Keywords Geology
Public URL https://hull-repository.worktribe.com/output/4270546

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Publisher Licence URL
http://creativecommons.org/licenses/by/4.0

Copyright Statement
© 2023 The Author(s). This is an Open Access article distributed under the terms of the Creative Commons Attribution 4.0 License (http://creativecommons.org/licenses/by/4.0/). Published by The Geological Society of London. Publishing disclaimer: www.geolsoc.org.uk/pub_ethics






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