The Huai’an area of Northwest Hebei Province stands on the central-north of the North China Craton (NCC). Zircon U-Pb, Lu-Hf isotope and trace elements compositions are analyzed. As a result, zircon cores with oscillatory zoning exhibit various 207Pb/206Pb ages in range of 2 542~1 902 Ma (1σ). They show a positive relations with Th/U (0.10~1.92) ratios, ΣHREE (59.1×10-6~452×10-6) and εHf(t) values, indicating their different degrees of lattice recrystallization due to the postdated metamorphism. Zircon grains with the most concordant and old ages yield a mean 207Pb/206Pb age of (2 471±18) Ma (2σ, MSWD=6.7). The authors interpret this age to be the age of granulite to amphibolite retrograde metamorphism. The Ti-in-zircon temperatures record their formation temperatures in range of 683~714 ℃ which are highly consistent with the temperatures from granulite to amphibolite retrograde metamorphism. Therefore, the isotopic ages of 1 850~1 800 Ma might be representative of the stage of regional crust uplift postdating the Late Palaeoproterozoic cratonization.