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- W2079002169 abstract "Abstract Correlation between cleavage formation and growth of syntectonic fibrous minerals is used to show that superposition of crenulation cleavages in Lower Ordovician rocks from the Eastern Townships of Quebec, Canada, resulted from overprinting during progressive deformation. Fibres of calcite, quartz and chlorite in pressure shadows adjacent to pyrite curve through almost 90°, from parallelism with the first to parallelism with the second, superposed crenulation cleavage. Whereas the cleavages mark only the initial and final orientations of the flattening plane, the fibres record the gradual rotation of this plane in the interval between formation of the cleavages. The continuity of the undeformed fibres suggests a single progressive deformation rather than two separate tectonic events." @default.
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- W2079002169 date "1980-06-01" @default.
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- W2079002169 title "Superposed crenulation cleavages resulting from progressive deformation" @default.
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- W2079002169 doi "https://doi.org/10.1016/0040-1951(80)90041-4" @default.
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