C–O–S and Pb isotopic data suggest a magma-related source.
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The Luping is a stratiform, bedding-plane fault-controlled epithermal polymetallic deposit.
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The Luping Pb deposit is a part of the Beiya porphyry Au (Cu)–Pb–Zn system.
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The Luping Pb deposit formed in the India–Eurasia post-collisional setting.
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