福建行洛坑高产热花岗岩U、Th来源与富集成因

胡鐇分; 刘昊; 王永; 刘向冲

doi:10.3799/dqkx.2024.088

Volume 50 Issue 4

Apr. 2025

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Hu Fanfen, Liu Hao, Wang Yong, Liu Xiangchong, 2025. U and Th Sources and Enrichment Mechanisms of High Heat Producing Granites in Xingluokeng, Fujian Province. Earth Science, 50(4): 1380-1400. doi: 10.3799/dqkx.2024.088

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Hu Fanfen, Liu Hao, Wang Yong, Liu Xiangchong, 2025. U and Th Sources and Enrichment Mechanisms of High Heat Producing Granites in Xingluokeng, Fujian Province. Earth Science, 50(4): 1380-1400. doi: 10.3799/dqkx.2024.088

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U and Th Sources and Enrichment Mechanisms of High Heat Producing Granites in Xingluokeng, Fujian Province

doi: 10.3799/dqkx.2024.088

Hu Fanfen^{1
,
,},
Liu Hao¹,
Wang Yong^{1, 2, 3},
Liu Xiangchong^{1, 2, 3
,
,}

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing 100081, China
3.
The Laboratory of Dynamic Diagenesis and Metallogenesis, Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

Received Date: 2024-06-12
Available Online: 2025-05-10
Publish Date: 2025-04-25

Abstract

Abstract

Tungsten deposit is genetically related to highly differentiated granites. The radioactive heat production of those tungsten-associated granites is mostly 5-10 μW•m^-3 and can be classified into high heat-producing granites. The radioactive heat mainly comes from U (70%), followed by Th (20%) and K (< 10%). The distribution pattern and genesis of heat-producing elements in tungsten granites are still unclear. The Xingluokeng large-scale tungsten deposit in Fujian Province was chosen as a typical case study. The main occurrence minerals of U, Th, and K were constrained using the principle of mass conservation, the compositional analysis of single minerals (biotite, plagioclase, zircon, monazite, and apatite), and published major and trace element data of the whole rock in the Xingluokeng granites. The zircon U-Pb ages of G1 and G2 are 151.5±0.6 Ma and 150.0±0.6 Ma, respectively. The total heat production rates of G1 and G2 calculated from single minerals are 1.78 μW•m^-3 and 2.28 μW•m^-3, respectively. Among them, K mainly occurs in K-feldspar and biotite, and the heat contribution rate of K of these two minerals to the whole rock is less than 10%. Th mainly comes from monazite, and the Th heat contribution rate in monazite is 46% at the highest. U mainly comes from zircon and monazite, and the heat contribution rate is less than 15%. The heat production rates of G1 and G2 minerals are 48% and 37% of the whole rock average heat production rates (3.74 μW•m^-3 and 6.10 μW•m^-3, respectively). This significant difference may be due to a large amount of U existing in a small amount of high-U zircon. Due to the limited statistical sampling of these high-U zircons, the calculated heat production rate from single minerals tends to be underestimated. The enrichment of U and Th in the Xingluokeng granites may be controlled by the protoliths and later crystallization differentiation.The decay heat from radioactive elements in the Xingluokeng granite (especially the late granite) may prolong the time limit of hydrothermal convection and promote the formation of scheelite.
- heat-producing elements,
- zircon,
- monazite,
- tungsten deposit,
- Xingluokeng,
- mineral deposits

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References(113)

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