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Fig. 1. Geologic map of the Godtha˚bsfjord region, compiled mainly from maps by Allaart (1982), Chadwick and Coe (1983, 1988),Garde (1987, 1989) and McGregor (1984), with terrane boundaries and Ikkattoq gneiss from McGregor et al
Fig. 2. Geologic map showing the location of Akilia within theregional tectonic framework, after Chadwick and Nutman(1979) and Chadwick and Coe (1983).
Fig. 4. Heterogeneous gneiss comprising layers of pegmatite-banded tonalitic and dioritic Amıˆtsoq gneiss (grey), parallellayers and boudins of amphibolite (black) derived from Amer-alik dykes, and pegmatite veins (white)
Fig. 5. Heterogeneous tonalitic and dioritic gneiss (Amıˆtsoqgneiss) with parallel layers of pegmatite-veined mafic andultramafic gneiss (Akilia association) and thin layers of amphi-bolite
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