Structural characteristics and Re-Os dating of quartz-pyrite veins in the Lewisian Gneiss Complex, NW Scotland: Evidence of an Early Paleoproterozoic hydrothermal regime during terrane amalgamation
Keywords: مجتمع لوئیس; Re-Os geochronology; Lewisian Complex; Palaeoproterozoic; Quartz-pyrite veins; Scourie dykes; Terranes;