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Projekt Druckansicht

The evolution of the crust-mantle system in the early Archean

Fachliche Zuordnung Mineralogie, Petrologie und Geochemie
Förderung Förderung von 2007 bis 2019
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 57914783
 
Erstellungsjahr 2022

Zusammenfassung der Projektergebnisse

Eoarchean mantle and mantle-derived rocks can provide primary information on geodynamic processes operating on the early Earth. This project has combined new petrological observations, comprehensive major and trace element data as well as Lu-Hf, Sm-Nd amd Re-Os isotope data of > 3.81 Ga ultramafic rocks from the Itsaq Gneiss Complex (IGC) in southern West Greenland. Lutetium-Hf whole rock age regression lines mainly yield Eoarchean ages of ca. 3.9 to 3.8 Ga, in good agreement with minimum ages inferred from field relationships (>3.8 Ga). Major and trace element signatures, the Lu-Hf isotope inventory as well as most major elements, MREE, HREE, and HFSE were only slightly disturbed during metamorphic overprint. Nearly flat primitive mantle-normalized REE patterns obtained for the mantle peridotites resemble those of refertilized modern abyssal peridotites and may reflect re-enrichment of initially depleted peridotite by melt-like subduction components, as also indicated by Th-HFSE-REE characteristics. We suggest that the compositions are best explained by partial hydrous melt depletion in the spinel stability field, followed by refertilization by low quantities of adakite-like melt. Altogether, the geochemical data can be put in the framework of a geodynamic model, where Eoarchean mantle underwent significant melt extraction and subsequent re-fertilization by subduction-like components. For the first time, combined platinum-group element (PGE) and Re-Os isotope data were measured on these peridotites showing that Re-depletion model ages are mostly Eoarchean, in accord with U-Pb zircon ages of crosscutting granitoid intrusives. PGE abundances and patterns are indistinguishable from those of modern depleted mantle peridotites. Abundances of Os, Ir and Ru combined with Os isotope compositions in the Greenland peridotites indicate that primitive, late-accreted material must have been efficiently mixed into the sampled mantle domains by Eoarchean time.

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