Volcanic arc affinity for charnockite and felsic gneiss from the Lützow–Holm Complex
Upper intercept ages of 2508–2490 Ma suggesting a Neoarchean arc magmatic event
Magma derivation from Meso- to Neoarchean juvenile components mixed with reworked crustal materials
551–584 Ma high-grade metamorphism related to a collisional event during Gondwana amalgamation
Fragments of Neoarchean and Early Neoproterozoic juvenile magmatic arcs in the complex