Geology and Isotope Geochemistry of the Dongzhongla Pb–Zn Deposit in Tibet: Implications for the Origin of the Ore‐Forming Fluids and Storage Condition of Certain Metals | Zendy

Fei Guang Chun | Zendy; Zhou Yu | Zendy; Deng Yun | Zendy; Chen Xu | Zendy; Wen Chun Qi | Zendy; Yu Qinglin | Zendy; Ding Feng | Zendy; Zhou Xiong | Zendy; Huo Yan | Zendy

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Geology and Isotope Geochemistry of the Dongzhongla Pb–Zn Deposit in Tibet: Implications for the Origin of the Ore‐Forming Fluids and Storage Condition of Certain Metals

Author(s) -

Fei Guang Chun,

Zhou Yu,

Deng Yun,

Chen Xu,

Wen Chun Qi,

Yu Qinglin,

Ding Feng,

Zhou Xiong,

Huo Yan

Publication year - 2018

Publication title -

resource geology

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 0.597

H-Index - 43

eISSN - 1751-3928

pISSN - 1344-1698

DOI - 10.1111/rge.12158

Subject(s) - geology , geochemistry , meteoric water , carbonate , calcite , pyrite , skarn , galena , δ34s , magmatic water , isotope geochemistry , crust , mantle (geology) , mineralogy , sphalerite , quartz , fluid inclusions , isotope , metallurgy , hydrothermal circulation , paleontology , physics , quantum mechanics , seismology , materials science

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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