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The volcanic zircons, inherited pre-magmatic core domains and hydrothermal zircons in felsic meta-volcanic rocks and Cu–Zn orebodies from the Neoarchean Hongtoushan deposit in China were distinguished according to their texture, 207Pb/206Pb ages, Th/U and oxygen isotopic ratios. Their respective element compositional and Lu–Hf isotopic features were studied using LA–(MC)–ICP–MS methods, showing that...
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