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Fig. 1. Location of the Kangerluluk volcano-sedimentary sequence and principal divisions of the Ketilidian Orogen (adapted fromGarde and Schønwandt, 1995) in southern Greenland
Fig. 2. Geology of the Kangerluluk volcano-sedimentary sequence with four identified lithofacies, a batholith phase and various sills.The feldspar-pyroxene sill/dykes are coeval with the volcano-sedimentary sequence, whereas the feldspar-magnetite sill is r
Fig. 3. Contact relationships between lithofacies and characteristics of synvolcanic dykes
Fig. 3. (Continued)
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