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Previous studies have shown that the 2.04 Ga Kangamiut dyke swarm of SW Greenland was injected into an active tectonic environment associated with the formation of the Nagssugtoqidian orogenic belt. Major and trace element modelling of the swarm shows that its chemical evolution was controlled by simple clinopyroxene-plagioclase fractionation. However, such trends - although typical of continental...