Fabric and kinematic study of the Bíteš orthogneiss (southwestern Moravia): Result of large-scale northeastward shearing parallel to the Moldanubian/Moravian boundary-Reference-Cited by-同舟云学术

Fabric and kinematic study of the Bíteš orthogneiss (southwestern Moravia): Result of large-scale northeastward shearing parallel to the Moldanubian/Moravian boundary

Published:1990-05 Issue:1-3 Volume:177 Page:229-244
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Schulmann Karel

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference42 articles.

1. Zur Geologie und Petrographie Moravischer Gesteine im Gebiet NW Weitersfeld, Niederosterreich;Bernroider,1986

2. Evolution of folds during progressive shear in the South Armorican shear zone;Berthe;J. Struct. Geol.,1980

3. Orthogneiss, mylonites and noncoaxial deformation of granites: the example of South Armorican shear zone;Berthe;J. Struct. Geol.,1979

4. The Himalayan Central Thrust pile and its quartz rich tectonites in Central Nepal;Bouchez;Tectonophysics,1981

5. Quartz fabric in shear-zone mylonites: evidence for a major imprint due to late strain increments;Brunel;Tectonophysics,1980

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