Crenulation cleavage differentiation: implications of solution-deposition processes
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2018, Journal of Structural GeologyCitation Excerpt :It is also possible that a similar fold of low amplitude and small decrease of volume in the limbs increases the amplitude by flattening, thus maintaining the similar form. Microfolds (crenulation), commonly associated with cleavage lamellae (crenulation cleavage), are a typical fabric of folded incompetent rocks (mainly slates or phyllites) with a previous strong planar mechanical anisotropy (e.g. slaty cleavage) (Cosgrove, 1976; Gray, 1977, 1979; Gray and Durney, 1979). The microfolds can be symmetrical or asymmetrical, and usually have a geometry close to that of a similar fold (e.g. Ramsay and Huber, 1987, p. 436).
Intracrystalline deformation of garnet, wollastonite and pectolite grains during development of a crenulation cleavage in the sheared skarn
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