Hongqiyingzi Group underwent episodic tectonothermal events from Archean to Phanerozoic.
TNCO Paleoproterozoic subduction at 1.95 Ga and collision at 1.85 Ga.
460–420 Ma concordant zircons record the onset of TNCO exhumation.
Ubiquitous 360–320 Ma concordant zircons reveal major period exhumation.
Young orogeny heavily triggered Archean crust and Paleoproterozoic orogen reactivation.