Isclinal fold in granulite-facies, garnet-bearing metasediments.The fold is truncated by a compositionally layered flaser gabbro of Permian age.
PhotoID442
Isclinal fold in granulite-facies, garnet-bearing metasediments.The fold is truncated by a compositionally layered flaser gabbro of Permian age.
PhotoID442
Photograph: Ivan Zibra
Reference: Reference: Zibra I, Kruhl JH, Braga R (2010). Late Palaeozoic deformation of post-Variscan lower crust: shear zone widening due to strain localization during retrograde shearing. Int J Earth Sci (Geol Rundsch) DOI 10.1007/s00531-009-0441-5