摘要
The northern Hebei Province is one major exposure region of Early Precambrian metamorphic basement of North China Craton. LA-ICP-MS zircon U-Pb and Lu-Hf isotopic analyses for the monzogranitic gneiss yield a discordant upper intercept age of (2 509 ± 10) Ma, reflecting its crystallization age. The geodynamic processes producing these Neoarchen granitic gneisses suggest that their tectonic background are analogous to the west coast of South America, implying a transitional geodynamic regime from convergent compression to back-arc extension in the northern Hebei Province.