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In-plane strip deformation can be neglected as the strips deform about 100× more easily towards the mirror than towards their neighbours due to their perforated center and their width/thickness aspect ratio of 8 (ref. 51).
If other rocks that are clearly not deformed can be found at the same site, the time of deformation can be inferred to lie between the absolute isotopic ages of the two units.
To some extent the deformation can be related to different tectonic settings.
The time of deformation can be bracketed, however, if datable units, which both predate and postdate it, can be identified.
Two types of deformation can be distinguished: compression and in-plane shear.
Hence, subroutines designed for standard models (continuous deformation) can be applied with only minor modifications necessary.
The effect of this deformation can be eliminated through the use of different methods.
We show that plastic deformation can be either homogeneous or heterogeneous, depending on the NW orientation.
The complete governing equations under the finite deformation can be derived from the physical variational principle.
With increasing corrosion damage, significant degradations in strength and deformation can be observed.
Since the particles are stiff compared to the embedding rubber, their deformation can be ignored for all practical purposes.
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