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- W2000532312 abstract "Abstract Microstructural study of foliated quartz cataclasites of a segment of the Towaliga fault zone, Georgia, USA, indicates that rock strain by cataclastic deformation occurred through microscopic displacements along a distributed system of shear bands. The localized cataclastic flow in the bands was in turn the result of frictional sliding along a network of mesoscopic shear fractures that accommodated initial strains and were in part created by high fluid pressures in the fault zone. The shear fractures at both the microscopic and mesoscopic scale were formed in the Riedel R1, P, and Y orientations. Simultaneous displacements along these Riedel shears produced the cataclastic foliation, rhomb-shaped and tabular quartz grain fabrics, and straight, stepped grain boundaries. Crystallization by fluids accompanied fracturing and possibly aided the cataclastic flow by forming muscovite and quartz crystals along fractures. Most fluid inclusion trails and quartz veins cut across the cataclastic features, indicating that fluids which assisted the deformation later healed the fractures. A right-lateral sense of displacement is suggested for the cataclastic flow, consistent with the kinematics of the mylonitization along the fault zone." @default.
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- W2000532312 date "1991-12-01" @default.
- W2000532312 modified "2023-09-26" @default.
- W2000532312 title "Initiation of cataclastic flow and development of cataclastic foliation in nonporous quartzites from a natural fault zone" @default.
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- W2000532312 doi "https://doi.org/10.1016/0040-1951(91)90006-e" @default.
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