The formation of Earth’s earliest continental crust during the Archean eon (4.0–2.5 Ga) reflects a complex interplay of mantle melting, magmatic differentiation and crustal recycling. Partial melting ...
The Archean eon witnessed the formation of Earth’s first stable continental nuclei, often preserved as cratonic terranes that record the geochemical pathways from primitive mafic protocrust to evolved ...
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