Continental evolution influenced by relamination of deeply subducted continental crust
Taras Gerya
Nature Geoscience, Published online: 05 May 2026; doi:10.1038/s41561-026-01963-w Post-collisional calc-alkaline magmatism has originated from the mixing and hybridization of relaminated continental crust and mantle peridotite since the Archaean, according to numerical simulations of continental subduction and melting experiments.