Inventory and assessment of palaeoarchaean gneiss terrains and detrital zircons in southern West Greenland

Geochemical methods to advance knowledge on the early Earth require supplies of well-preserved >3600 Ma rocks and minerals (e.g. zircon). One of the most important resources for these are small domains within high metamorphic grade Palaeoarchaean gneisses in the Archaean Craton, southern West Greenland. In the Nuuk region these gneisses occur as two terranes (totalling ∼3000 km 2) with differences in their pre-3600 Ma histories, and they are tectonically separated from each other by younger rocks. In the north is the Isukasia terrane (early metamorphic grade amphibolite facies). It is devoid of pre-3600 Ma in situ partial melt and contains locally well-preserved 3690 and 3810 Ma tonalites, ≥3810 Ma ultramafic rocks plus the tectonically composite Isua supracrustal belt with some locally well-preserved ∼3800 and 3710 Ma volcanic and sedimentary materials. To the south is the Færingehavn terrane (up to granulite facies in the Palaeoarchaean) that is dominated by 3850-3660 Ma migmatites containing variable amounts of in situ 3660-3600 Ma partial melt. Akilia island in this terrane contains some ∼3850 Ma tonalites, mafic and sedimentary rocks - the world's oldest-known sediments. Domains of lower total strain and anatexis on some of other islands near Akilia has left small amounts of well-preserved 3850 Ma tonalite. There are two less known smaller bodies of Palaeoarchaean rocks north of the Nuuk region. The Qarliit Tasersuat assemblage consists of polyphase, migmatitic gneisses with lenses of mafic and siliceous rocks. Two SHRIMP zircon dates reveal 3600-3700 Ma rocks, strongly affected by ∼3600 and 2770 Ma metamorphisms. The Aasivik terrane also consists of polyphase migmatitic gneisses, and previous SHRIMP U/Pb zircon reconnaissance dating of three samples found components up to ∼3600 Ma old with strong reworking in 2720-2550 Ma events. The West Greenland Archaean Craton is a collage of Palaeo- to Neoarchaean terranes, assembled in several Archaean events. Metasediments within post-Palaeoarchaean terranes are devoid of ≥3600 Ma detritus, but are dominated by zircons of the same age as major crust-forming TTG suites of their terrane. Metasediments along terrane boundaries, even those in contact with Palaeoarchaean terranes, contain very few (