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• W2042374059 abstract "Sandstone layers within tightly chevron-folded quartz-rich turbidites of the Lachlan Fold belt southeastern Australia show a fanning spaced cleavage overprinted by a non-fanning grain alignment cleavage, low internal strains recorded by quartz grain separations (XZ ≈ 1.4−1.8) and low fold flattening strains (XZ < 1.8). Angular relations between spaced cleavage and bedding in folds with varying tightness suggest that sandstone layers initially act as stress-supporting members with spaced cleavage development due to pressure solution taking place at limb dips up to 15°. During fold development sandstone layers undergo rigid body rotation involving interlayer slip without marked internal deformation except at fold hinges. After fold lock-up bedding-spaced cleavage angles change due to inner arc collapse by pressure solution and subsequent flattening with formation of a grain alignment cleavage and mica beard growth. Internal deformation of sandstone is characterized by microstructures related to solution-redeposition processes and growth of mica. Chevron folds form by homogeneous shortening and pressure solution due to layer-parallel shortening, tangential longitudinal strain due to buckling, fold tightening by inner arc collapse due to pressure solution and fold flattening at metamorphic peak with growth of mica. Geometric modelling of internal strains and bedding-cleavage angles requires a significant component of interlayer slip during chevron fold development under greenschist facies conditions." @default.
• W2042374059 created "2016-06-24" @default.
• W2042374059 creator A5038145024 @default.
• W2042374059 creator A5075098249 @default.
• W2042374059 date "1994-10-01" @default.
• W2042374059 modified "2023-09-27" @default.
• W2042374059 title "Strain, cleavage and microstructure variations in sandstone: implications for stiff layer behaviour in chevron folding" @default.
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• W2042374059 doi "https://doi.org/10.1016/0191-8141(94)90002-7" @default.
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