Abstract
More than 90% of the tungsten resources of China are in the Nanling region of South China, and the Yaogangxian vein deposit is the largest tungsten deposit in this region. The tungsten deposits have ages of 150–160 Ma, and are spatially, temporally and genetically related to granites which were previously believed to be produced by crustal anatexis. This paper provides He and Ar isotope data of fluid inclusions in pyrite and arsenopyrite from the Yaogangxian W veins. 3He/4He ratios range from 0.41 to 3.03 Ra (where Ra is the 3He/4He ratio of air = 1.39 × 10−6), and 40Ar/36Ar ratios from 328 to 1,191. Moreover, there are excellent correlations between He and Ar isotopic compositions. The results suggest that the ore-forming fluids are a mixture between a crustal fluid containing atmospheric Ar and crustal 4He and a fluid containing mantle components. It is likely that the former is a low temperature meteoric fluid, and the later is a fluid exsolved from the W-associated granitic magma, which formed by crustal melting induced by intrusion of a mantle-derived magma.
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Acknowledgements
The field work was supported by the Yaogangxian Mine Company. The authors are grateful to Dr. Lehmann B. and Prof. Zhou M.F. for their constructive comments on this manuscript, and to Turner G. and Kendrick M.A. for their thoughtful reviews. This research was financially supported by the National Basic Research Program of China (973 Program) (2007CB411408) and the National Natural Science Foundation of China (40903023).
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Hu, RZ., Bi, XW., Jiang, GH. et al. Mantle-derived noble gases in ore-forming fluids of the granite-related Yaogangxian tungsten deposit, Southeastern China. Miner Deposita 47, 623–632 (2012). https://doi.org/10.1007/s00126-011-0396-x
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DOI: https://doi.org/10.1007/s00126-011-0396-x