Metamorphic evolution of Daqingshan supracrustal rocks and garnet granite from the North China Craton: Constraints from phase equilibria modelling, geochemistry, and SHRIMP U–Pb geochronology

•The pre-peak, peak, post-peak near-ITD and cooling stages have been identified.•The protolith of the Daqingshan supracrustal rocks formed at ~2.5 Ga.•Anatexis of Daqingshan supracrustal rocks occurred during ~2.43–2.40 Ga.•The formation of garnet granite related to Late Neoarchean tectono-thermal event.