湘中杏枫山金钨矿床成因: 热液磷灰石U-Pb定年和原位S同位素制约

娄元林; 刘贤红; 曾昊; 郑卓; 刘德亮; 马慧敏; 马盈

doi:10.3799/dqkx.2024.059

Volume 49 Issue 12

Dec. 2024

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Lou Yuanlin, Liu Xianhong, Zeng Hao, Zheng Zhuo, Liu Deliang, Ma Huimin, Ma Ying, 2024. Genesis of Xingfengshan Au-W Deposit in Central Hunan Province: Constraints from Hydrothermal Apatite U-Pb Dating and In Situ S Isotopes. Earth Science, 49(12): 4265-4277. doi: 10.3799/dqkx.2024.059

Citation:

Lou Yuanlin, Liu Xianhong, Zeng Hao, Zheng Zhuo, Liu Deliang, Ma Huimin, Ma Ying, 2024. Genesis of Xingfengshan Au-W Deposit in Central Hunan Province: Constraints from Hydrothermal Apatite U-Pb Dating and In Situ S Isotopes. Earth Science, 49(12): 4265-4277. doi: 10.3799/dqkx.2024.059

Citation:

Lou Yuanlin, Liu Xianhong, Zeng Hao, Zheng Zhuo, Liu Deliang, Ma Huimin, Ma Ying, 2024. Genesis of Xingfengshan Au-W Deposit in Central Hunan Province: Constraints from Hydrothermal Apatite U-Pb Dating and In Situ S Isotopes. Earth Science, 49(12): 4265-4277. doi: 10.3799/dqkx.2024.059

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Genesis of Xingfengshan Au-W Deposit in Central Hunan Province: Constraints from Hydrothermal Apatite U-Pb Dating and In Situ S Isotopes

doi: 10.3799/dqkx.2024.059

Lou Yuanlin^{1, 2, 3
,
,},
Liu Xianhong¹,
Zeng Hao¹,
Zheng Zhuo¹,
Liu Deliang⁴,
Ma Huimin⁴,
Ma Ying^{4
,
,}

1.
Changsha Natural Resources Comprehensive Survey Center, China Geological Survey, Changsha 410600, China
2.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
4.
Collaborative Innovation Center for Exploration of Strategic Mineral Resources, School of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2024-04-07
Available Online: 2025-01-09
Publish Date: 2024-12-25

Abstract

Abstract

Xingfengshan is a representative gold-tungsten deposit in the Xiangzhong metallogenic belt. The age of gold mineralization, the source of ore-forming metals and the genesis of the deposit are still controversial. Based on detailed petrographic observation and LA-(MC)-ICP-MS analysis, in situ U-Pb dating of hydrothermal apatite and in situ S-isotope analysis of arsenopyrite in the auriferous quartz veins are carried out in this paper to constrain the age of gold mineralization, trace the source of ore-forming metals, and deepen the understanding of the genesis of the deposit. The U-Pb age of hydrothermal apatite in gold-bearing quartz veins is 215.1±7.5 Ma, which is consistent with the intrusion age of the Baimashan complex. The δ³⁴S values of arsenopyrite are centrally distributed between -9.2‰ to -7.7‰, indicating that the ore-forming metal is derived from a mixture of magmatic-hydrothermal fluids and host rocks.. The study shows that the W mineralization and Au mineralization of the Xingfengshan deposit occurred in the Late Triassic, and both may be the products of magmatic activities of the Baimashan igneous complex, and the Xingfengshan deposit should belong to the intrusion-related gold deposit.
- hydrothermal apatite U-Pb dating,
- in situ S isotope,
- Xingfengshan Au-W deposit,
- Xiangzhong metallogenic belt,
- intrusion-related gold deposit,
- deposits

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