江西虎圩金铅锌矿床矿物化学、流体包裹体特征及地质意义

抄尉尉; 许德如; 李增华; 陈立泉; 周先军; 袁波; 杨立飞; 陈加杰; 张健

doi:10.3799/dqkx.2022.305

Volume 49 Issue 4

Apr. 2024

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Article Navigation > Earth Science > 2024 > 49(4): 1292-1306

Chao Weiwei, Xu Deru, Li Zenghua, Chen Liquan, Zhou Xianjun, Yuan Bo, Yang Lifei, Chen Jiajie, Zhang Jian, 2024. Characteristics and Geological Implications of Mineral Chemistry and Fluid Inclusions in Huxu Au-Pb-Zn Ore Deposit, Jiangxi Province. Earth Science, 49(4): 1292-1306. doi: 10.3799/dqkx.2022.305

Citation:

Chao Weiwei, Xu Deru, Li Zenghua, Chen Liquan, Zhou Xianjun, Yuan Bo, Yang Lifei, Chen Jiajie, Zhang Jian, 2024. Characteristics and Geological Implications of Mineral Chemistry and Fluid Inclusions in Huxu Au-Pb-Zn Ore Deposit, Jiangxi Province. Earth Science, 49(4): 1292-1306. doi: 10.3799/dqkx.2022.305

Citation:

Chao Weiwei, Xu Deru, Li Zenghua, Chen Liquan, Zhou Xianjun, Yuan Bo, Yang Lifei, Chen Jiajie, Zhang Jian, 2024. Characteristics and Geological Implications of Mineral Chemistry and Fluid Inclusions in Huxu Au-Pb-Zn Ore Deposit, Jiangxi Province. Earth Science, 49(4): 1292-1306. doi: 10.3799/dqkx.2022.305

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Characteristics and Geological Implications of Mineral Chemistry and Fluid Inclusions in Huxu Au-Pb-Zn Ore Deposit, Jiangxi Province

doi: 10.3799/dqkx.2022.305

1.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
2.
School of Earth Sciences, East China University of Technology, Nanchang 330013, China
3.
No.1 Geological Party of Jiangxi Nonferrous Metals Geological Exploration Bureau, Yingtan 335003, China

Received Date: 2022-03-31
Available Online: 2024-04-30
Publish Date: 2024-04-25

Abstract

Abstract

To study the genesis of ore deposits in the Dongxiang volcanic basin, the Huxu Au-Pb-Zn deposit was selected as the research object, and a detailed study of quartz trace elements, fluid inclusions thermometry and chemical compositions of chlorite was carried out. The results indicate that the main element substitution mechanism is Al³⁺+Li⁺ = Si⁴⁺.The pH of the ore-forming fluids is fluctuated episodically. The fluid inclusions are mainly gas-liquid type. The chlorite formed in an environment with relatively high sulfur fugacity and low oxygen fugacity. The ore-forming temperature is estimated to be 210-280 ℃.Combined with previous studies, it suggests that the Huxu deposit evolved with varying mixing ratio of magmatic fluids and meteoric water, accompanied by fluid-rock interaction, leading to the precipitation of ore veins in the opening fractures. The Huxu deposit is considered as epithermal deposit, with buried porphyry body.
- trace element of quartz,
- fluid inclusion,
- chlorite,
- Huxu Au-Pb-Zn deposit,
- Dongxiang volcanic basin,
- ore deposit geology

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References(60)

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Characteristics and Geological Implications of Mineral Chemistry and Fluid Inclusions in Huxu Au-Pb-Zn Ore Deposit, Jiangxi Province

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