Alexandra Tamas
New onshore insights into the role of structural inheritance during Mesozoic opening of the Inner Moray Firth Basin, Scotland
Tamas, Alexandra; Holdsworth, Robert E.; Underhill, John R.; Tamas, Dan M.; Dempsey, Edward D.; Hardman, Kit; Bird, Anna; McCarthy, Dave; McCaffrey, Ken J.W.; Selby, David
Authors
Robert E. Holdsworth
John R. Underhill
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
Dave McCarthy
Ken J.W. McCaffrey
David Selby
Contributors
Dr Eddie Dempsey E.Dempsey@hull.ac.uk
Project Member
Dr Anna Bird A.Bird@hull.ac.uk
Project Member
Abstract
The Inner Moray Firth Basin (IMFB) forms the western arm of the North Sea trilete rift system that initiated mainly during the Late Jurassic–Early Cretaceous with the widespread development of major NE–SW-trending dip-slip growth faults. The IMFB is superimposed over the southern part of the older Devonian Orcadian Basin. The potential influence of older rift-related faults on the kinematics of later Mesozoic basin opening has received little attention, partly owing to the poor resolution of offshore seismic reflection data at depth. New field observations augmented by drone photography and photogrammetry, coupled with U–Pb geochronology, have been used to explore the kinematic history of faulting in onshore exposures along the southern IMFB margin. Dip-slip north–south-to NNE–SSW-striking Devonian growth faults are recognized that have undergone later dextral reactivation during NNW–SSE extension. The U–Pb calcite dating of a sample from the synkinematic calcite veins associated with this later episode shows that the age of fault reactivation is 130.99 ± 4.60 Ma (Hauterivian). The recognition of dextral-oblique Early Cretaceous reactivation of faults related to the underlying and older Orcadian Basin highlights the importance of structural inheritance in controlling basin-to sub-basin-scale architectures and how this influences the kinematics of IMFB rifting.
Citation
Tamas, A., Holdsworth, R. E., Underhill, J. R., Tamas, D. M., Dempsey, E. D., Hardman, K., Bird, A., McCarthy, D., McCaffrey, K. J., & Selby, D. (2022). New onshore insights into the role of structural inheritance during Mesozoic opening of the Inner Moray Firth Basin, Scotland. Journal of the Geological Society, 179(2), Article 066. https://doi.org/10.1144/jgs2021-066
Journal Article Type | Article |
---|---|
Acceptance Date | Sep 27, 2021 |
Online Publication Date | Oct 12, 2021 |
Publication Date | Mar 1, 2022 |
Deposit Date | Oct 13, 2021 |
Publicly Available Date | Oct 14, 2021 |
Journal | Journal of the Geological Society |
Print ISSN | 0016-7649 |
Electronic ISSN | 2041-479X |
Publisher | Geological Society |
Peer Reviewed | Peer Reviewed |
Volume | 179 |
Issue | 2 |
Article Number | 066 |
DOI | https://doi.org/10.1144/jgs2021-066 |
Keywords | Geology |
Public URL | https://hull-repository.worktribe.com/output/3853626 |
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Copyright Statement
© 2021 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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