Evolution of folds during progressive shear in the South Armorican shear Zone, France-Reference-Cited by-同舟云学术

Evolution of folds during progressive shear in the South Armorican shear Zone, France

Published:1980-01 Issue:1-2 Volume:2 Page:127-133
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Berthé D.,Brun J.P.

Publisher

Elsevier BV

Subject

Geology

Reference22 articles.

1. Orthogneiss, mylonite and non-coaxial deformation of granites: the example of the South Armorican Shear Zone;Berthé;J. Struct. Geol.,1979

2. Orientations préférentielles du quartz et orthogneissification progressive en régime cisaillant: l'exemple du cisaillement sud-armoricain;Berthé;Bull. Soc. fr. Minér. & Cristallogr.,1979

3. Variably oriented co-planar primary folds;Borradaile;Geol. Mag.,1972

4. Significance of lineation and minor folds near major thrust faults in the Southern Appalachians and the British and Norwegian Caledonides;Bryant;Geol. Mag.,1969

5. The effects of folding on the C-axis fabrics of a quartz mylonite;Carreras;Tectonophysics,1977

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