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Petrogenesis of the Neoarchean Granitoid Gneisses in Northern Hebei Province
详细信息   
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.

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