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Meta-igneous (non-gneissic) tonalites and quartz-diorites from an extensive ca. 3800 Ma terrain south of the Isua supracrustal belt, southern West Greenland: constraints on early crust formation

Southern West GreenlandEngineeringGreenstone BeltIsua Supracrustal BeltGeologyCrustal MeltingGeochemistryEarly Crust FormationGeochronologyPetrologyCrust-mantle InteractionIgneous PetrologyEarth ScienceTectonics