Ore-forming mechanism of Huxu Au-dominated polymetallic deposit in the Dongxiang Basin, South China: Constraints from in-situ trace elements and S–Pb isotopes of pyrite

Author:

Gao Hongze,Chen JiajieORCID,Leng Chengbiao,Hu Yuhui,Xie Huidan,Li Zenghua

Funder

National Natural Science Foundation of China

State Key Laboratory for Nuclear Resources and Environment, East China Institute of Technology

Natural Science Foundation of Jiangxi Province

Publisher

Springer Science and Business Media LLC

Reference67 articles.

1. Bi XW, Hu RZ, Peng JT, Wu KX (2004) REE and HFSE geochemical characteristics of pyrites in Yao’an gold deposit: Tracing ore forming fluid signatures. Bull Min Petrol Geochem 23(1):1–4 (in Chinese with English abstract).

2. Cai YT, Ni P, Shen K, Zhu XT, Huang SJ, Zhang XC, Xu JH (2011) Study on the fluid inclusion from Dongxian copper deposit Jiangxi Province China. Acta Petrol Sin 27(5):1375–1386 (in Chinese with English abstract).

3. Cai YT, Ni P, Wang GG, Pan JY, Zhu XT, Chen H, Ding JY (2016) Fluid inclusion and H-O–S–Pb isotopic evidence for the Dongxiang Manto-type copper deposit, South China. J Geochem Explor 171:71–82. https://doi.org/10.1016/j.gexplo.2016.01.019

4. Cao GS, Zhang Y, Chen HY (2023) Trace elements in pyrite from orogenic gold deposits implications for metallogenic mechanism. Acta Petrol Sin 39(8):2330–2346 (in Chinese with English abstract). https://doi.org/10.18654/1000-0569/2023.08.06

5. Chen YJ, Ni P, Fan HR, Pirajno F, Lai Y, Su WC, Zhang H (2007) Diagnostic fluid inclusions of different types hydrothermal gold deposits. Acta Petrol Sin 23(9):2085–2108 (in Chinese with English abstract).

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