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- W1985206557 abstract "Synopsis The Loch Tay Fault in the Central Highlands of Scotland is the easternmost of six major faults that transect the Dalradian. Examination of the limited exposure along the sub-vertical fault walls in the type area demonstrates that it has undergone a history of left-lateral strike-slip as well as dip-slip. Evidence from the displacement of formation boundaries and of fold traces shows that the fault has undergone a finite history of 6.5–7.5 km of left-lateral strike-slip and a dip-slip, down to the NW, of 750–1000 m in the SW and central area, diminishing to 200 m or less in the NE. A major fault lens to the NW of the main fault (the Braes of Foss Fault Complex) has similarly undergone dip-slip (but down to the SE) and left-lateral strike-slip; however, two fault lenses to the SE of the major fault (the Glen Goulandie Fault Complex and a smaller lens to its SW) and associated splays have undergone right-lateral displacement. Displacements on the Frenich Burn Fault, a minor fault to the east of the Loch Tay Fault, are again dominantly left-lateral with small displacements down to the NW, whereas faults in an adjacent mine pit illustrate that displacements in the country rock are dominantly dip-slip. By analogy with the Tyndrum Fault, the main left-lateral and dip-slip movements are considered to be pre-Devonian, whereas the right-lateral and late extensional movements are interpreted as Carboniferous." @default.
- W1985206557 created "2016-06-24" @default.
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- W1985206557 date "2003-11-01" @default.
- W1985206557 modified "2023-10-05" @default.
- W1985206557 title "The Loch Tay Fault: type section geometry and kinematics" @default.
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- W1985206557 doi "https://doi.org/10.1144/sjg39020135" @default.
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