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• W2011049287 abstract "Foliated cataclasite and breccia exposed along a segment of the Towaliga fault zone (TFZ) in western Georgia, U.S.A., formed during two episodes of cataclastic deformation. Conventional KAr crystallization ages of muscovite collected along fractures in the foliated cataclasite at Dixon Mountain, suggest that following mylonitization, at about 296 Ma (Pennsylvanian), rocks along the TFZ were elevated upward across the 300°C isothermal surface and ductile deformation via cataclastic flow was initiated. Fluid inclusion microthermometry and quartz microfabric in the cataclasite suggest that the temperature during this first cataclastic deformation, which probably occurred at a depth greater than 8 km, was between 140 and 300°C. At around 237 Ma (Late Permian), cataclastic deformation was dominated by brecciation and extensive vein sealing and formed the silicified breccias at Dixon Mountain. Muscovites from another cataclastic segment of the TFZ give a relatively low apparent age of around 269 Ma, probably because of loss of argon or mixing with younger neocrystallized muscovite during cataclasis." @default.
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• W2011049287 date "1991-01-01" @default.
• W2011049287 modified "2023-10-16" @default.
• W2011049287 title "Timing and temperature of cataclastic deformation along segments of the Towaliga fault zone, western Georgia, U.S.A." @default.
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• W2011049287 doi "https://doi.org/10.1016/0191-8141(91)90044-j" @default.
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