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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.

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 Thumbnail


Authors

T. A. G. Utley

G. A. Blackbourn

E. Dempsey

R. A. Strachan

A. C. Morton

A. F. Bird

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. G., Holdsworth, R. E., Blackbourn, G. A., Dempsey, E., Strachan, R. A., McCaffrey, K. J. W., …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), https://doi.org/10.1144/jgs2022-148

Journal Article Type Article
Acceptance Date Feb 17, 2023
Online Publication Date Apr 27, 2023
Publication Date May 5, 2023
Deposit Date Aug 16, 2023
Publicly Available Date Aug 16, 2023
Journal Journal of the Geological Society
Print ISSN 0016-7649
Electronic ISSN 2041-479X
Publisher The Geological Society
Peer Reviewed Peer Reviewed
Volume 180
Issue 3
DOI https://doi.org/10.1144/jgs2022-148
Keywords Geology
Public URL https://durham-repository.worktribe.com/output/1719651

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