Source and Evolution of the Ore-Forming Fluids of Carlin-Type Gold Deposit in the Youjiang Basin, South China: Evidences from Solute Data of Fluid Inclusion Extracts

Xiaoye Jin; Chengfu Yang; Jianzhong Liu; Wu Yang

doi:10.1007/s12583-020-1055-x

Volume 32 Issue 1

Mar 2021

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Journal of Earth Science > 2021 > 32(1): 185-194.

Xiaoye Jin, Chengfu Yang, Jianzhong Liu, Wu Yang. Source and Evolution of the Ore-Forming Fluids of Carlin-Type Gold Deposit in the Youjiang Basin, South China: Evidences from Solute Data of Fluid Inclusion Extracts. Journal of Earth Science, 2021, 32(1): 185-194. doi: 10.1007/s12583-020-1055-x

Citation:

Xiaoye Jin, Chengfu Yang, Jianzhong Liu, Wu Yang. Source and Evolution of the Ore-Forming Fluids of Carlin-Type Gold Deposit in the Youjiang Basin, South China: Evidences from Solute Data of Fluid Inclusion Extracts. Journal of Earth Science, 2021, 32(1): 185-194. doi: 10.1007/s12583-020-1055-x

Citation:

Xiaoye Jin, Chengfu Yang, Jianzhong Liu, Wu Yang. Source and Evolution of the Ore-Forming Fluids of Carlin-Type Gold Deposit in the Youjiang Basin, South China: Evidences from Solute Data of Fluid Inclusion Extracts. Journal of Earth Science, 2021, 32(1): 185-194. doi: 10.1007/s12583-020-1055-x

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Source and Evolution of the Ore-Forming Fluids of Carlin-Type Gold Deposit in the Youjiang Basin, South China: Evidences from Solute Data of Fluid Inclusion Extracts

doi: 10.1007/s12583-020-1055-x

Xiaoye Jin^{1, 2
,
,
,},
Chengfu Yang^{2, 3},
Jianzhong Liu^{2, 3},
Wu Yang⁴

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Engineering Technology Innovation Center of Mineral Resources Explorations in Bedrock Zones, Ministry of Natural Resources, Guiyang 550081, China
3.
105 Geological Party, Guizhou Bureau of Geology and Mineral Exploration & Development, Guiyang 550018, China
4.
School of Resources and Environmental Engineering, Guizhou Institute of Technology, Guiyang 550003, China

More Information

Corresponding author: Xiaoye Jin, xiaoye.jin@cug.edu.cn
Received Date: 26 Jun 2020
Accepted Date: 07 Jul 2020
Publish Date: 01 Feb 2021

Abstract

Abstract

The source and evolution of ore-forming fluids is important to understand the genesis of Carlin-type gold deposit. Constraints on the source and evolution of ore fluid components by the conventional geochemical methods have long been a challenge due to the very fine-grained nature and complex textures of hydrothermal minerals in these deposits. In this study,we present the crush-leach analyzed solute data of fluid inclusion extracts within quartz,calcite,realgar,and fluorite from the Shuiyindong,Nibao,and Yata gold deposits in the Youjiang Basin,providing new insights into the source and evolution of ore-forming fluids. The results show that the high molar Cl/Br ratios up to 2 508 in fluid inclusion extracts are indicative of a contribution of magmatic hydrothermal fluids. Fluids mixing between basinal and magmatic-hydrothermal fluids are evident on the plots of Cl/Br versus Na/K ratios,showing that ore-stage milky quartz near the magmatic-hydrothermal fluids reflects magma origin of the ore-forming fluids,whereas late ore-stage drusy quartz and realgar near the defined basinal fluids suggest the later input of basinal fluids in late-ore stage. Although the predominately host rocks in Shuiyindong,Nibao and Yata gold deposit are bioclastic limestone,sedimentary tuff,and calcareous siltstone,respectively,the solute data of fluid inclusion extracts records they underwent the similar fluid-rocks reactions between the Na-rich magmatic hydrothermal fluids and the Ca- and Mg-rich host rocks. This study highlights the solute data of fluid inclusion extracts obtained by crush-leach analyses have the potential to fingerprint the source and evolution of ore-forming fluids of the Carlin-type gold deposit.
- solute data,
- fluid inclusion,
- source and evolution of ore-forming fluids,
- Carlin-type gold deposit,
- Youjiang Basin

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References(49)

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