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The E-W trending Nanling Range, located in the southern part of the South China Block (SCB), is characterized by widespread intra-continental Mesozoic granitoids and accompanying W–Sn polymetallic ore deposits. Detailed studies are presented on trace elements, U–Pb ages and Lu–Hf isotopes in zircons from the Mesozoic A2-type like granitoids (including the Qianlishan, Qitianling, Xianghualing, Huashan,...
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