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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

The timing and significance of mid-crustal shearing and exhumation of amphibolite facies 1 rocks along the Great Glen Fault Zone, Scotland 2 3 Thumbnail


Authors

R D Law

J R Thigpen

C Mako

A Kylander-Clark

M J Caddick

L R Moore

C Becker

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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