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.