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Voluminous Neoproterozoic igneous rocks along the western margin of the Yangtze Block, South China, provide an ideal opportunity for examining the nature of the mantle source, petrogenesis of the felsic plutons and processes and timing of crustal growth. The Dadukou, Tongde, Gaojiacun and Shaba mafic plutons, and Datian and Dajianshan adakitic plutons were selected for zircon Lu–Hf isotope analysis...
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