High- and Low-MgO tonalitic and trondhjemitic gneisses in the Tangtu-Majuanzi area.
Partial melting of the subducted slabs and the juvenile lower crust.
Three episodes of magmatism at ∼2680 Ma, ∼2600–2570 Ma and ∼2550–2510 Ma.
A Neoarchaean active continental margin in the North Liaoning area.