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• W1987254249 abstract "The widely cited Sibson-Scholz conceptual fault zone model suggests that seismically active, upper crustal brittle faults pass downward across a predominantly thermally controlled transition at 10–15 km depth into ductile shear zones in which deformation occurs by aseimic viscous creep. The crustal-scale Outer Hebrides Fault Zone (OHFZ) in NW Scotland has been described as the type example of such a continental fault zone. It cuts Precambrian basement gneisses and is deeply exhumed, allowing direct study of the deformation products and processes that occur across a wide range of crustal depths. A number of fault rock assemblages are recognized to have formed during a long-lived displacement history lasting in excess of 1000 Myr. During Caledonian movements that are recognized along much of the 190 km onshore fault trace, brittle, cataclasite-bearing faults in the west of the OHFZ are unequivocally overprinted to the east by a younger fabric related to a network of ductile shear zones. Field observations and regional geochronological data demonstrate that there is no evidence for reheating of the fault zone due to thrust-related crustal thickening or shear heating. Microstructural observations show that the onset of viscous deformation was related to a major influx of hydrous fluids. This led to retrogression, with the widespread development of new finegrained phyllosilicate-bearing fault rocks (“phyllonites”), and the onset of fluid-assisted, grain size-sensitive diffusional creep in the most highly deformed and altered parts of the fault zone. Phyllonitic fault rocks also occur in older, more deeply exhumed parts of the fault zone, implying that phyllonitization had previously occurred at an earlier stage and that this process is possible over a wide temperature (depth) range within crustal-scale faults. Our data provide an observational basis for recent theoretical and experimental studies which suggest that crustal-scale faults containing interconnected networks of phyllosilicate-bearing fault rocks will be characterized by long-term relative weakness and shallow (∼5 km) frictional-viscous transition zones. Similar processes acting at depth may provide an explanation for the apparent weakness of presently active structures such as the San Andreas Fault." @default.
• W1987254249 created "2016-06-24" @default.
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• W1987254249 date "2001-10-01" @default.
• W1987254249 modified "2023-10-14" @default.
• W1987254249 title "A reappraisal of the Sibson-Scholz fault zone model: The nature of the frictional to viscous (“brittle-ductile”) transition along a long-lived, crustal-scale fault, Outer Hebrides, Scotland" @default.
• W1987254249 cites W1963987887 @default.
• W1987254249 cites W1968718505 @default.
• W1987254249 cites W1969706851 @default.
• W1987254249 cites W1974036238 @default.
• W1987254249 cites W1976909487 @default.
• W1987254249 cites W1979229404 @default.
• W1987254249 cites W1982637158 @default.
• W1987254249 cites W1987117634 @default.
• W1987254249 cites W1988064976 @default.
• W1987254249 cites W1992759889 @default.
• W1987254249 cites W1993516950 @default.
• W1987254249 cites W1999025317 @default.
• W1987254249 cites W1999518605 @default.
• W1987254249 cites W2003578564 @default.
• W1987254249 cites W2007765396 @default.
• W1987254249 cites W2008324928 @default.
• W1987254249 cites W2011939763 @default.
• W1987254249 cites W2012384607 @default.
• W1987254249 cites W2012471105 @default.
• W1987254249 cites W2015399809 @default.
• W1987254249 cites W2015488510 @default.
• W1987254249 cites W2019386742 @default.
• W1987254249 cites W2021138049 @default.
• W1987254249 cites W2022547621 @default.
• W1987254249 cites W2025571789 @default.
• W1987254249 cites W2028154812 @default.
• W1987254249 cites W2035698766 @default.
• W1987254249 cites W2036193373 @default.
• W1987254249 cites W2038083893 @default.
• W1987254249 cites W2042154180 @default.
• W1987254249 cites W2042767874 @default.
• W1987254249 cites W2042921659 @default.
• W1987254249 cites W2042983533 @default.
• W1987254249 cites W2048578916 @default.
• W1987254249 cites W2051841330 @default.
• W1987254249 cites W2055706694 @default.
• W1987254249 cites W2056032867 @default.
• W1987254249 cites W2056332463 @default.
• W1987254249 cites W2058060723 @default.
• W1987254249 cites W2065110848 @default.
• W1987254249 cites W2066293722 @default.
• W1987254249 cites W2069530996 @default.
• W1987254249 cites W2073687371 @default.
• W1987254249 cites W2073741756 @default.
• W1987254249 cites W2077521920 @default.
• W1987254249 cites W2086308009 @default.
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• W1987254249 cites W2103440685 @default.
• W1987254249 cites W2116225973 @default.
• W1987254249 cites W2116330848 @default.
• W1987254249 cites W2124309231 @default.
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• W1987254249 cites W2133071671 @default.
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• W1987254249 cites W2135987837 @default.
• W1987254249 cites W2147476711 @default.
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• W1987254249 cites W2164683099 @default.
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• W1987254249 doi "https://doi.org/10.1029/2000tc001250" @default.
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