Petrochemistry and tectonic significance of gneiss-amphibolite-migmatite association of Khuda metamorphic core complex, Southeastern Desert, Egypt.
The general tectonic frame work of the metamorphic rock assemblage in the Wadi Khuda are, SE Desert of Egypt, is a major doubly plunging running in the NE-SW direction. This assemblage comprises paragneisses , flecked gneisses, migmatites and intercalated with amphibolite lenses. Field data combined with petrographic description indicate that the degree of metamorphism increases toward the core of the ... Read more