The birth of a cratonic nucleus: Lithogeochemical evolution of the 4.02-2.94 Ga Acasta Gneiss Complex
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文摘

Here we present new mapping of the Acasta Gneiss Complex based on age and chemistry.

The oldest components were formed in petrogenetic environments similar to Iceland.

Typical Archean continental crust does not appear until 3.6 Ga.

Zircon geochemistry indicates the involvement of surface waters.

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