Geochemical evidence for reworking of the juvenile crust in the Neoarchean for felsic magmatism in the Yunzhongshan area, the North China Craton

•The felsic igneous rocks in the Lüliang complex were formed at 2.56–2.50 Ga.•The TTG gneisses and felsic volcanics were produced by partial melting of the moderately enriched arc crust.•The high-K granites were produced by partial melting of the arc crust similar to modern IAB.•Both 2.8–2.7 Ga and 2.6–2.5 Ga magmatic events were related to oceanic subduction.