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- W2016091339 abstract "The morphology and microstructure of individual crenulation cleavages are dependent on a complex interplay of the physical conditions, the pre-existing fabric and the operative deformation mechanisms. Controlling factors are neither readily observable nor obtainable from the final cleavage microfabric. However, observable features such as the metamorphic grade, the microfolding, the pre-existing fabric and the cleavage microstructure provide some information on the parameters which affect differentiation in crenulated rocks. The pre-existing fabric is probably the singlemost important factor affecting the morphology and microstructure of crenulation cleavages. This fabric essentially predetermines the geometry of the associated crenulation folds, the mineralogy of the cleavage and the type of fabric modification associated with the development of the cleavage. The metamorphic grade broadly specifies the pressure-temperature boundary conditions (i.e., the field in stress-temperature space) for crenulation deformations. Since crenulation cleavages are most common under greenschist facies conditions or lower, the conditions favoured most for cleavage development are probably temperatures below 450°C and pressures ranging from 2 kb to 10 kb (cf. Turner, 1968, p. 366). The microfolding does not determine the type of crenulation cleavage which develops, but it does determine their location in a crenulated fabric and the spacing of the cleavages. The cleavage microstructure indirectly provides information on the strain mechanisms responsible for development of the cleavages as finite structures. Observations indicate that solution processes play an important part in crenulation cleavage development." @default.
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- W2016091339 title "Some Parameters Which Affect the Morphology of Crenulation Cleavages" @default.
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- W2016091339 doi "https://doi.org/10.1086/628361" @default.
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