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Journal ArticleDOI

The effects of folding on the C-axis fabrics of a quartz mylonite

TLDR
In this paper, the development of a stable c-axis fabric pattern in quartz-mylonites from the Cap de Creus shear zones is summarized and the subsequent effects of fold development on these fabrics is analyzed in more detail.
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This article is published in Tectonophysics.The article was published on 1977-04-20. It has received 194 citations till now. The article focuses on the topics: Slip (materials science) & Transverse plane.

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Journal ArticleDOI

S-C Mylonites

TL;DR: Berthe et al. as mentioned in this paper proposed two types of foliations in mylonites and mylonitic rocks: (a) S-surfaces related to the accumulation of finite strain and (b) C-surface related to displacement discontinuities or zones of relatively high shear strain.
Journal ArticleDOI

Shear zone geometry: A review

TL;DR: In this article, the authors classified brittle, brittle-ductile, and ductile shear zones into three classes: brittle, ductile and polygonal shear regions, and established the geometry and displacement boundary conditions of these zones.
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On mylonites in ductile shear zones

TL;DR: In this paper, the development of mylonite microstructures and fabrics are discussed from this point of view and seven possible softening processes are discussed: superplasticity, geometrical softening, continual recrystallization, reaction softening and chemical softening.
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Development of sheath folds in shear regimes

TL;DR: In this paper, the development of three-dimensional fold shapes in shear regimes is studied using theoretical and experimental methods and with reference to natural examples, and three models are presented for their development, two invoking flow with steady stream lines, the third involving unsteadiness accompanying boudinage.
References
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Electron Microscopy of Thin Crystals

TL;DR: Hirsch et al. as mentioned in this paper described further experiments on the preparation of thin film sections of embedded Backscatter Kikuchi diffraction in the SEM for identification of crystallographic thin films by electron microscopy.
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Strain variation in shear belts

TL;DR: In rocks deformed by natural orogenic processes, it is usual to find that the finite strain state varies from locality to locality as mentioned in this paper, and in some deformed rocks high strain states are localized within app...
Journal ArticleDOI

Development of internal structures in deformed anisotropic rocks

TL;DR: In this article, the behavior during deformation of composite foliated rocks is discussed in terms of the "average" rheological properties of the rock, not the properties of individual components.