“…The Rhiconich and Assynt blocks are separated by the Laxford Shear Zone (Evans, 1965;Corfu et al, 1994;Goodenough et al, 2010;. The central region may be further subdivided into Assynt and Gruinard blocks, separated by the Canisp Shear Zone (Coward and Park, 1987;Chattopadhyay et al, 2010;Goodenough et al, 2010). The Assynt block features TTG gneisses and metamorphosed mafic and ultramafic lithologies, some of which display granulite mineral assemblages formed during the Badcallian (Park, 1970).…”