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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