Who coined the alternative name regarding a geological concept of the orogenic belt that was active in Gondwanaland?
Samfrau Orogeny The Samfrau Geosyncline or Samfrau Orogeny is an orogenic belt that was active in the Palaeozoic and early Mesozoic in Gondwanaland, formed by small terranes and deep accumulations of old sediment dumped off the continent's edge by erosion, acccreting against the Pacific-side coast of Gondwanaland due to subduction. Its name (as "Samfrau Geosyncline") was coined by Alexander du Toit. Parts of it exist now in northern Argentina, South Africa, Antarctica, and part of the east coast region of Australia, as shown in the map at this link.
Hebridean Terrane The Hebridean Terrane is one of the terranes that form part of the Caledonian orogenic belt in northwest Scotland. Its boundary with the neighbouring Northern Highland Terrane is formed by the Moine Thrust Belt. The basement is formed by Archaean and Paleoproterozoic gneisses of the Lewisian complex, unconformably overlain by the Neoproterozoic Torridonian sediments, which in turn are unconformably overlain by a sequence of Cambro–Ordovician sediments. It formed part of the Laurentian foreland during the Caledonian continental collision.