Alexandra Tamas
Unravelling the Sequence and Timing of Fault-Related Deformation in Superimposed Rift Basins, Inner Moray Firth, NE Scotland
Tamas, Alexandra; Holdsworth, Robert E.; Tamas, Dan M.; Dempsey, Edward D.; Hardman, Kit; Bird, Anna; Underhill, John R.; McCarthy, Dave; McCaffrey, Ken J. W.; Selby, David
Authors
Robert E. Holdsworth
Dan M. Tamas
Dr Eddie Dempsey E.Dempsey@hull.ac.uk
Senior Lecturer in Structural Geology and Geohazards
Kit Hardman
Dr Anna Bird A.Bird@hull.ac.uk
Reader in Geology
John R. Underhill
Dave McCarthy
Ken J. W. McCaffrey
David Selby
Abstract
Devonian rocks of the Palaeozoic Orcadian Basin are well exposed along the northern flanks of the younger Mesozoic to Cenozoic Inner Moray Firth Basin in Scotland. These rocks preserve a succession of structures related to superimposed rifting and inversion events spanning nearly 400 Myrs. We combine new detailed field observations augmented by drone photography and the creation of 3D digital outcrops, coupled with U-Pb geochronology of syn-faulting calcite-mineralized veins to better constrain the absolute timing of fault movements and decipher the kinematic history of basin opening and inversion.Using this approach, we were able to isolate characteristic structures, fault kinematics, fault rock development and associated mineralization types related to five regional deformation events: (1) Devonian transtensional rifting associated to sinistral Great Glan Fault movements leading to the development of the Orcadian Basin; (2) Late Carboniferous inversion related to dextral Great Glen Fault reactivation; (3) minor N-S, possibly Permian calcite veins; (4) Late Jurassic–Early Cretaceous rifting related to the development of the IMFB; and finally, (5) Cenozoic uplift, reactivation, and local inversion. Our study demonstrates the utility of microstructurally constrained U-Pb geochronology of fault-related calcite mineralization. Applied elsewhere, our methodology has the potential to give consistent and regionally significant new insights into the nature and timing of superimposed rift-related deformation processes worldwide.
Citation
Tamas, A., Holdsworth, R. E., Tamas, D. M., Dempsey, E. D., Hardman, K., Bird, A., Underhill, J. R., McCarthy, D., McCaffrey, K. J. W., & Selby, D. (2025). Unravelling the Sequence and Timing of Fault-Related Deformation in Superimposed Rift Basins, Inner Moray Firth, NE Scotland. Lithosphere, 2024(Special15), Article 183. https://doi.org/10.2113/2024/lithosphere_2024_183
Journal Article Type | Article |
---|---|
Acceptance Date | Feb 25, 2025 |
Online Publication Date | Apr 21, 2025 |
Publication Date | Apr 21, 2025 |
Deposit Date | Jun 4, 2025 |
Publicly Available Date | Jun 19, 2025 |
Journal | Lithosphere |
Print ISSN | 1941-8264 |
Electronic ISSN | 1947-4253 |
Publisher | GeoScienceWorld |
Peer Reviewed | Peer Reviewed |
Volume | 2024 |
Issue | Special15 |
Article Number | 183 |
DOI | https://doi.org/10.2113/2024/lithosphere_2024_183 |
Public URL | https://hull-repository.worktribe.com/output/5132074 |
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Copyright Statement
Copyright © 2025. Alexandra Tamas et al.
Exclusive License GeoScienceWorld. Distributed under a Creative Commons Attribution License (CC BY 4.0).