S and Pb isotopic compositions of the Qianchuiliu Gold Deposit on the northeastern margin of the Jiaolai Basin: Implication on the source of ore-forming material

Han Xiaomeng; Guo Yuncheng; Duan Liuan; Wang Jiantian; Zhao Pengfei; Wang Lipeng; Yu Guangming

doi:10.19509/j.cnki.dzkq.tb20220659

Volume 42 Issue 3

May 2023

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Article Navigation > Bulletin of Geological Science and Technology > 2023 > 42(3): 210-221

Han Xiaomeng, Guo Yuncheng, Duan Liuan, Wang Jiantian, Zhao Pengfei, Wang Lipeng, Yu Guangming. S and Pb isotopic compositions of the Qianchuiliu Gold Deposit on the northeastern margin of the Jiaolai Basin: Implication on the source of ore-forming material[J]. Bulletin of Geological Science and Technology, 2023, 42(3): 210-221. doi: 10.19509/j.cnki.dzkq.tb20220659

Citation:

Han Xiaomeng, Guo Yuncheng, Duan Liuan, Wang Jiantian, Zhao Pengfei, Wang Lipeng, Yu Guangming. S and Pb isotopic compositions of the Qianchuiliu Gold Deposit on the northeastern margin of the Jiaolai Basin: Implication on the source of ore-forming material[J]. Bulletin of Geological Science and Technology, 2023, 42(3): 210-221. doi: 10.19509/j.cnki.dzkq.tb20220659

Citation:

Han Xiaomeng, Guo Yuncheng, Duan Liuan, Wang Jiantian, Zhao Pengfei, Wang Lipeng, Yu Guangming. S and Pb isotopic compositions of the Qianchuiliu Gold Deposit on the northeastern margin of the Jiaolai Basin: Implication on the source of ore-forming material[J]. Bulletin of Geological Science and Technology, 2023, 42(3): 210-221. doi: 10.19509/j.cnki.dzkq.tb20220659

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S and Pb isotopic compositions of the Qianchuiliu Gold Deposit on the northeastern margin of the Jiaolai Basin: Implication on the source of ore-forming material

doi: 10.19509/j.cnki.dzkq.tb20220659

1.
Yantai Geological Survey Center of Coastal Zone, China Geological Survey, Yantai Shandong 264000, China
2.
Ministry of Natural Resources Technology Innovation Center for Deep Gold Resources Exploration and Mining/Shandong Provincial Engineering Laboratory of Application and Development of Big Data for Deep Gold Exploration, Weihai Shandong 264209, China
3.
Command Center of Natural Resources Comprehensive Survey, China Geological Survey, Beijing 100032, China

Received Date: 25 Nov 2022

Abstract

Abstract

The Qianchuiliu Gold Deposit on the northeastern margin of the Jiaolai Basin is a newly discoverd altered rock type gold deposit, and is a medium-sized gold deposit hosted in the structural alteration zone between Muniushan, Jingshan Group and Queshan monzonitic granites. However, the source of ore-forming materials and the ore genesis are not clear. Based on previous field and analytical studies, the authors conducted sulfur and lead isotopic analyses on gold-bearing pyrite from typical ores as the research target. The δ³⁴S values are high and homogeneous ranging from 10.13‰-12.39‰, with an average of 10.98‰ and polar odds of 2.26‰. These sulfur isotopic results reveal a mixing process of sulfur in the Jingshan Group during the upwelling of deep ore-forming fluid. The ratios of ²⁰⁶Pb/²⁰⁴Pb, ²⁰⁷Pb/²⁰⁴Pb, and ²⁰⁸Pb/²⁰⁴Pb vary from 17.149-18.886, 15.482-15.677, and 37.860-40.073, respectively, suggesting a crust-mantle mixed source. In conclusion, sulfur and lead isotope analysis results of the Qianchuiliu Gold Deposit show a crust-mantle mixed source and are similar to those of typical gold deposits in this region. The gold deposits on the northeastern margin of the Jiaolai Basin formed at the large-scale Yanshanian metallogenic event, indicating great prospecting potential in this area.
- northeastern margin of the Jiaolai Basin,
- Qianchuiliu Gold Deposit,
- sulfur isotope,
- lead isotope,
- material source

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References(46)

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S and Pb isotopic compositions of the Qianchuiliu Gold Deposit on the northeastern margin of the Jiaolai Basin: Implication on the source of ore-forming material

doi: 10.19509/j.cnki.dzkq.tb20220659

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S and Pb isotopic compositions of the Qianchuiliu Gold Deposit on the northeastern margin of the Jiaolai Basin: Implication on the source of ore-forming material

doi: 10.19509/j.cnki.dzkq.tb20220659

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