Earth SciencesNature Communications
Archaean continental crust formed from mafic cumulates
M. A. Smit, K. A. Musiyachenko, et al.
This study delves into the origins of the Archaean continental crust, specifically the TTG component. It uncovers that these primary TTGs emerged from the melting of specialized rocks deep within proto-continental roots. Conducted by Matthijs A. Smit, Kira A. Musiyachenko, and Jeroen Goumans, it challenges traditional views by eliminating the need for external influences like meteorite impacts.
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