Timothy Brendan Armitage timothy.b.armitage@durham.ac.uk
PGR Student Doctor of Philosophy
Late Carboniferous dextral transpressional reactivation of the crustal-scale Walls Boundary Fault, Shetland: the role of pre-existing structures and lithological heterogeneities
Armitage, Timothy B.; Watts, Lee M.; Holdsworth, Robert E.; Strachan, Robin A.
Authors
Lee M. Watts
Professor Bob Holdsworth r.e.holdsworth@durham.ac.uk
Professor
Robin A. Strachan
Abstract
The Walls Boundary Fault (WBF) in Shetland, Scotland, formed during the Ordovician-Devonian Caledonian orogeny and underwent dextral reactivation in the Late Carboniferous. In a well-exposed section at Ollaberry, westerly verging, gently plunging regional folds in the Neoproterozoic Queyfirth Group on the western side of the WBF are overprinted by faults and steeply-plunging Z-shaped brittle-ductile folds that indicate contemporaneous right-lateral and top-to-the W reverse displacement. East of the WBF, the Early Silurian Graven granodiorite complex exhibits fault-parallel fractures with Riedel, P and conjugate shears indicating N-S striking dextral deformation and an additional contemporaneous component of E-W shortening. In the Queyfirth Group, the structures are arranged in geometrically and kinematically distinct fault-bounded domains that are interpreted to result from two superimposed tectonic events, the youngest of which displays evidence for bulk dextral transpressional strain partitioning into end-member wrench and contractional strain domains. During dextral transpressional deformation, strain was focussed into pelite horizons and favourably aligned pre-existing structures, leaving relics of older deformation in more competent lithologies. This study highlights the importance of pre-existing structures and lithological heterogeneity during reactivation and suggests the development of a regional transpressional tectonic environment during the Late Carboniferous on the Shetland Platform.
Citation
Armitage, T. B., Watts, L. M., Holdsworth, R. E., & Strachan, R. A. (2020). Late Carboniferous dextral transpressional reactivation of the crustal-scale Walls Boundary Fault, Shetland: the role of pre-existing structures and lithological heterogeneities. Journal of the Geological Society, 178, Article jgs2020-078. https://doi.org/10.1144/jgs2020-078
Journal Article Type | Article |
---|---|
Acceptance Date | Sep 22, 2020 |
Online Publication Date | Sep 30, 2020 |
Publication Date | Oct 23, 2020 |
Deposit Date | Sep 28, 2020 |
Publicly Available Date | Dec 3, 2020 |
Journal | Journal of the Geological Society |
Print ISSN | 0016-7649 |
Electronic ISSN | 2041-479X |
Publisher | The Geological Society |
Peer Reviewed | Peer Reviewed |
Volume | 178 |
Article Number | jgs2020-078 |
DOI | https://doi.org/10.1144/jgs2020-078 |
Public URL | https://durham-repository.worktribe.com/output/1291553 |
Files
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Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/
Copyright Statement
© 2020 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/).
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