Origin of the Luping Pb deposit in the Beiya area, Yunnan Province, SW China: Constraints from geology, isotope geochemistry and geochronology
文摘

C–O–S and Pb isotopic data suggest a magma-related source.

The Luping is a stratiform, bedding-plane fault-controlled epithermal polymetallic deposit.

The Luping Pb deposit is a part of the Beiya porphyry Au (Cu)–Pb–Zn system.

The Luping Pb deposit formed in the India–Eurasia post-collisional setting.

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