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Review of Survey Activities 2005: Using zircon geochronology to resolve the Archaean geology of southern West Greenland

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Figure 1 shows the distribution of known supracrustal belts in the Godthåbsfjord region, typically comprising high-grade metamorphic volcanic, ultramafic, subordinate aluminous and siliceous sedimentary rocks
Fig. 4. Detrital zircon populations linked to the distribution of supracrustal belts.
Fig. 5. Pegmatite on Storø cross-cutting and deformed by the Storø shear zone fabric, and Neoarchaean supracrustal amphibolite host rock.

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