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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