Flanking fold showing antithetic displacement in high-grade quartzites and schists (Priestely Schists); Simpson Cgraggs, Norhern Victoria Land (Ross Orogen, Antarctica). The cross-cutting element is a granite vein related to the Cambrian-Ordovician Granite Harbour Intrusives.
PhotoID233
Flanking fold showing antithetic displacement in high-grade quartzites and schists (Priestely Schists); Simpson Cgraggs, Norhern Victoria Land (Ross Orogen, Antarctica). The cross-cutting element is a granite vein related to the Cambrian-Ordovician Granite Harbour Intrusives.
PhotoID233
Photograph: R. Carosi
Reference: R. Carosi – Unipi