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• W2020586206 abstract "Thin sheets of composite ice-mica have been deformed in order to simulate the development of cleavages in quartz-mica rocks. A strong initial mica preferred orientation was variably oriented to the shortening direction. Deformation parallel to the foliation results in a crenulation type cleavage developing from shear bands initiated after a component of pure shear. Deformation oblique to the foliation produces a differentiated cleavage and involves a large component of shear strain subparallel to the original anisotropy. The strain is accommodated by intra- and intercrystalline processes that produce extensive grain elongation and rearrangement of the ductile matrix, thereby forming ice vs mica rich regions. On the other hand, there is no drastic morphological change when a sample is shortened perpendicular to an original foliation: that is, where the micas lie in the plane of no shear strain. Instead, the mica fabric is strengthened and the grains in the ductile matrix are flattened. Two models are presented for the initiation, propagation and evolution of the observed crenulation versus differentiated cleavage types. These depend on mica stacking and orientation relative to the transverse properties of the sample and also on the direction of anisotropy to the XY plane of the bulk strain ellipsoid. The models invoke shear on planes of high shear strain and rotation of the shear bands and rigid mica grains into a direction approximately parallel to the bulk extension direction." @default.
• W2020586206 created "2016-06-24" @default.
• W2020586206 creator A5048584901 @default.
• W2020586206 date "1984-01-01" @default.
• W2020586206 modified "2023-10-14" @default.
• W2020586206 title "Shear bands, crenulations and differentiated layering in ice-mica models" @default.
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• W2020586206 doi "https://doi.org/10.1016/0191-8141(84)90054-3" @default.
• W2020586206 hasPublicationYear "1984" @default.
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