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Numerous U–Pb zircon geochronological data show that rocks of the Precambrian basement from the North China craton (NCC) have two age peaks at 1.8–1.9 and ∼2.5Ga, respectively. Whether the most prominent peak at ∼2.5Ga really registered a period of major crustal growth in the NCC thus making it different from the global major crustal growth period of ∼2.7Ga is uncertain. In this paper, we carried...
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