| The pure shear deformation seen in the movies produces a sub-horizontal foliation defined by an alignment of grain shapes. Many of the original grains, both in the movies and in the FLAC model below that displayed higher order birefringence colours have disappeared. This reflects the development of a more permissive preferred-orientation within the sample and the evolution of a new fabric |
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| Figure 1. 4. 1. Polycrystalline
aggregate showing: Undeformed shape of grains and slip-plane
traces and initial random two-dimensional orientation of slip-plane normal
(c-axes) with respect to the specimen orientation. Deformed
by 29% shortening, the grains in the aggregate show elongation parallel
to the extension direction and the c-axes are concentrated in a
bi-symmetrical pattern about the shortening axis. This 2D FLAC model is
taken from Wilson & Zhang (1996). |
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| A two-dimensional view of Undeformed grains in a polycrystalline aggregate and slip-plane traces and initial random orientation of slip-plane normal (c-axes). Deformed aggregate shows grain-shape alignment parallel to the extension direction and the c-axes are concentrated in a bi-symmetrical pattern about the shortening axis. |
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| Figure 1.4.3.
The c-axis distributions in pure shear versus a simple shear regime. |
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Created: August 23, 1999 Last modified: March 15, 2004 Authorised by: Head, School of Earth Sciences Property of School of Earth Sciences - The University of Melbourne - Australia. Disclaimer and copyright. Design and maintained by Hadi Sim (hadims@unimelb.edu.au) |
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