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Archaean continental crust formed from mafic cumulates - Nature Communications

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Archaean continental crust formed from mafic cumulates - Nature Communications

Large swaths of juvenile crust with tonalite-trondhjemite-granodiorite (TTG) composition were added to the continental crust from about 3.5 billion years ago. Although TTG magmatism marked a pivotal step in early crustal growth and cratonisation, the petrogenetic processes, tectonic setting and sources of TTGs are not well known. Here, we investigate the composition and petrogenesis of Archaean TTGs using high field-strength-element systematics.

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Archaean continental crust formed from mafic cumulates - Nature Communications

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Archaean continental crust formed from mafic cumulates - Nature Communications

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