R D Law
The timing and significance of mid-crustal shearing and exhumation of amphibolite facies 1 rocks along the Great Glen Fault Zone, Scotland 2 3
Law, R D; Thigpen, J R; Mako, C; Kylander-Clark, A; Caddick, M J; Moore, L R; Becker, C; Holdsworth, R E; Strachan, R A; Leslie, A G
Authors
J R Thigpen
C Mako
A Kylander-Clark
M J Caddick
L R Moore
C Becker
Professor Bob Holdsworth r.e.holdsworth@durham.ac.uk
Professor
R A Strachan
A G Leslie
Abstract
The Rosemarkie Inlier lies on the NW side of the Great Glen Fault Zone (GGFZ) and is composed of foliated and lineated Lewisian gneisses and Moine metasedimentary rocks. The mylonitic foliation strikes NE-SW (parallel to the GGFZ), dips steeply SE and contains a gently- moderately plunging mineral lineation. Microstructural and quartz c-axis fabric analyses indicate that oblique sinistral shearing occurred under amphibolite facies conditions. LA-ICPMS analyses on monazite rims in the gneisses yield 206 Pb/ 238 U ages of 401.8±4.8 Ma (including 2σ uncertainty and a propagated additional 1% external uncertainty). Similar deformation and recrystallization temperatures indicated by quartz fabrics (610 °C) and monazite-xenotime thermometry (616±25°C), respectively, in the gneisses suggests that ductile sinistral shearing was ongoing at c. 402 Ma. The c. 402 Ma rim age is the
youngest monazite age recorded in the Northern Highland Terrane (NHT) and indicates that sinistral shearing at mid-crustal
levels was ongoing along the GGFZ in Lower Devonian (Emsian, 407 393 Ma) times when the thrust sheets of the NHT to the
NW had already been exhumed. The Rosemarkie basement rocks are unconformably overlain by Middle Devonian (Eifelian,
393 387 Ma) sedimentary rocks, indicating time-averaged exhumation rates of c. 1.75 mm a 1 between 402 and c. 390 Ma,
assuming a geothermal gradient of 30°C km 1.
.
Citation
Law, R. D., Thigpen, J. R., Mako, C., Kylander-Clark, A., Caddick, M. J., Moore, L. R., Becker, C., Holdsworth, R. E., Strachan, R. A., & Leslie, A. G. (2025). The timing and significance of mid-crustal shearing and exhumation of amphibolite facies 1 rocks along the Great Glen Fault Zone, Scotland 2 3. Journal of the Geological Society, 182(4), Article jgs2024-264. https://doi.org/10.1144/jgs2024-264
Journal Article Type | Article |
---|---|
Acceptance Date | Apr 9, 2025 |
Online Publication Date | Apr 18, 2025 |
Publication Date | May 27, 2025 |
Deposit Date | Jun 25, 2025 |
Publicly Available Date | Jun 26, 2025 |
Journal | Journal of the Geological Society |
Print ISSN | 0016-7649 |
Electronic ISSN | 2041-479X |
Publisher | The Geological Society |
Peer Reviewed | Peer Reviewed |
Volume | 182 |
Issue | 4 |
Article Number | jgs2024-264 |
DOI | https://doi.org/10.1144/jgs2024-264 |
Public URL | https://durham-repository.worktribe.com/output/4122598 |
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Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/
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