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Aug 12, 2024 · A popular conceptual tectonic model envisages the Great Glen Fault to be part of a sinistral strike-slip system active during the mid-Silurian through early Devonian with c. 700 km of displacement.
Sep 13, 2024 · A popular conceptual tectonic model envisages the Great Glen Fault to be part of a sinistral strike-slip system active during the mid-Silurian to early Devonian with c. 700 km of displacement.
The Great Glen Fault: the swinging pendulum of displacement estimates. The striking geomorphological aspect of the Great Glen of Scotland is its ruler-straight NE–SW trend for 200 km defined by a relatively narrow, steep-sided valley with hundreds of metres of relief.
The Great Glen hosts the most prominent fault in the British Isles, the Great Glen Fault. It originated towards the end of the Caledonian Orogeny (around 430-390 million years ago), and cuts diagonally across the Highlands from Fort William to Inverness.
Aug 25, 2021 · The Great Glen is a remarkably straight, fault-controlled, steep-sided and glacially overdeepened trench that is clearly visible from space and separates the Northern Highlands and Grampian Highlands geological terranes (Chap. 2).
- Jon W. Merritt, Clive A. Auton
- 2021
Aug 6, 2024 · Abstract: A popular conceptual tectonic model envisages the Great Glen Fault to be part of a sinistral strike-slip system active during the mid-Silurian through early Devonian with c. 700 km of displacement. Here we use sedimentological, geochemical and detrital zircon age data to show that restoring 250–300 km of displacement suffices to ...
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The Great Glen Fault Zone is a major, subvertical, reactivated fault within the Scottish Caledonides. Post-Caledonian dextral movements of a few tens of kilometres have been demonstrated previously from the displacement of geological markers.