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We report here the whole-rock Hf–Nd isotopic data on Mesozoic–Cenozoic basaltic lavas from Liaoning, Shandong, Hebei and Jiangsu–Anhui regions in the North China Craton (NCC). These lavas can be readily subdivided into two groups. The older (>110Ma) lavas are relatively depleted in high field strength elements (HFSEs), and have enriched Sr–Nd–Hf isotopic compositions. The younger (<110Ma) lavas,...
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