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As a newly discovered medium‐sized deposit, the Dongzhongla skarn Pb–Zn deposit is located in the northern margin of the eastern Gangdese, central Lhasa block. Based on the ore‐forming geological conditions in this deposit, H, O, C, S, Pb, Sr, He, Ne, and Ar isotopic compositions were analyzed. According to basic skarn mineralogy, the economic metals, and the origin of the ore‐forming fluids, the Dongzhongla deposit was classified as a skarn‐type Pb–Zn deposit.

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