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- W2146572212 abstract "Synopsis In the Ullapool to Strath Kanaird region of the NW Highlands the thrusts of the Moine thrust zone generally show a foreland propagating sequence but there are important anomalies. The Moine thrust itself appears to be a late structure, slicing across the earlier thrust stacks. There are several ages of normal fault movement. An early set formed synchronous with thrusting and involved extension in a WNW–ESE direction, parallel to general thrust transport, but also extension NE–SW, perpendicular to thrusting. These variations in movement indicate non-plane strain conditions, with important implications for section restoration. The early normal faults are either cut by or decouple on the Sole thrust to the Moine thrust system. There are late normal faults however, which are well-developed in the Ullapool area, and these are probably Mesozoic in age." @default.
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- W2146572212 date "1988-06-01" @default.
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- W2146572212 title "The thrust and normal faults of the Ullapool–Strath Kanaird region and their implications for NW Highland tectonics" @default.
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- W2146572212 doi "https://doi.org/10.1144/sjg24010035" @default.
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