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• W2007644927 abstract "In the ductile regions of orogenic wedges, late “brittle” structures formed at shallow crustal depths have received little attention. However, they are important as they of ten record the final stages in deformational history during uplift and erosion of the orogen. In the Moine rocks of Sutherland, late Caledonian brittle folds and low-angle faults post-date ductile structures formed during WNW-NW-directed thrust movements earlier in the same orogenic event. In the western Moine Nappe, the late structures display geometries which indicate that they formed during regionally ESE-directed extensional movements, down the dip of the pre-existing regional foliation. These late structures are correlated with similar, WNW-directed extensional low-angle faults recognised in the Moine Thrust Zone south of the Assynt culmination. Both are thought to have formed in response to late Caledonian gravity-induced thinning of the Moine Thrust wedge, and both pre-date Devonian extension associated with the formation of the West Orkney Basin. Along-strike changes in the location and sense of extensional movements, north and south of the Assynt culmination, are explained by changes in the pre-existing structural geometry of the Caledonian ductile thrust nappes within the Moine. Hence, earlier deformation patterns are thought to exert important controls over later events in an evolving orogenic wedge." @default.
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• W2007644927 creator A5008832725 @default.
• W2007644927 date "1989-12-01" @default.
• W2007644927 modified "2023-10-16" @default.
• W2007644927 title "Late brittle deformation in a caledonian ductile thrust wedge: new evidence for gravitational collapse in the Moine Thrust sheet, Sutherland, Scotland" @default.
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• W2007644927 doi "https://doi.org/10.1016/0040-1951(89)90100-5" @default.
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