Fig. 7

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Structures in migmatite: a) Metaxitic amphibolite with a continuous network of leucosome veins concordant to discordant to the syn-migmatitic foliation; b) Metatexite with a texturally continuous network of leucosome veins delineating the syn-migmatitic foliation, isoclinal folds and shear zones; c) Asymmetric metatexite boudins in heterogeneous granite (or diatexite); d) Asymmetric synmigmatitic (viscous) folds; e) Texturally continuous network of leucosome veins delineating the syn-nmigmatitic foliation and a dextral shear zone; f) syn-migmatitic strike-slip fault; g) Metatexite raft with folded leucosome in textural continuity with the heterogeneous granite (or diatexite); h) texturally continuous network of leucosome veins delineating the syn-migmatitic foliation, folds and shear zones; i) Metatexite with syn-migmatitic foliation marked by concordant leucosome in textural continuity with discordant leucosome localized in shear zones.
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