赣南会昌辉石闪长岩中磷灰石和锆石的年代学、成因矿物学及铀成矿指示意义

曾认宇; 潘家永; 苏惠; 甘德斌; 钟福军; 杜后发; 严杰; 张辰光

doi:10.3799/dqkx.2022.127

Volume 48 Issue 9

Sep. 2023

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Article Navigation > Earth Science > 2023 > 48(9): 3258-3279

Zeng Renyu, Pan Jiayong, Su Hui, Gan Debin, Zhong Fujun, Du Houfa, Yan Jie, Zhang Chenguang, 2023. Geochronology and Genetic Mineralogy of Apatite and Zircon from the Huichang Pyroxene Diorite in Southern Jiangxi Province: Implications for Uranium Mineralization. Earth Science, 48(9): 3258-3279. doi: 10.3799/dqkx.2022.127

Citation:

Zeng Renyu, Pan Jiayong, Su Hui, Gan Debin, Zhong Fujun, Du Houfa, Yan Jie, Zhang Chenguang, 2023. Geochronology and Genetic Mineralogy of Apatite and Zircon from the Huichang Pyroxene Diorite in Southern Jiangxi Province: Implications for Uranium Mineralization. Earth Science, 48(9): 3258-3279. doi: 10.3799/dqkx.2022.127

Citation:

Zeng Renyu, Pan Jiayong, Su Hui, Gan Debin, Zhong Fujun, Du Houfa, Yan Jie, Zhang Chenguang, 2023. Geochronology and Genetic Mineralogy of Apatite and Zircon from the Huichang Pyroxene Diorite in Southern Jiangxi Province: Implications for Uranium Mineralization. Earth Science, 48(9): 3258-3279. doi: 10.3799/dqkx.2022.127

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Geochronology and Genetic Mineralogy of Apatite and Zircon from the Huichang Pyroxene Diorite in Southern Jiangxi Province: Implications for Uranium Mineralization

doi: 10.3799/dqkx.2022.127

Zeng Renyu^{1, 2, 3
,
,},
Pan Jiayong^{1, 2},
Su Hui^{1, 2},
Gan Debin^{1, 2},
Zhong Fujun^{1, 2},
Du Houfa^{1, 2},
Yan Jie^{1, 2},
Zhang Chenguang⁴

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.
Department of Earth Sciences, Durham University, Durham DH1 3LE, UK
4.
School of Geographic Sciences, Xinyang Normal University, Xinyang 464000, China

Received Date: 2022-03-06
Available Online: 2023-10-07
Publish Date: 2023-09-25

Abstract

Abstract

The spatial and temporal distribution of Mesozoic mantle-derived magma in South China is closely related with the metallogenic model of the granite-type uranium deposit. However, it has always been an important yet difficult issue of studies to explain the origin of zircon in mantle-derived magma and clarify the emplacement age of mantle-derived magma. Focusing on a newly discovered mantle-derived pyroxene diorite in the Huichang area, southern Jiangxi Province, this paper presents a systematic study on its mineralogy, mineral geochemistry, chronology and bulk geochemistry. The Huichang pyroxene diorite is characterized by SiO₂ contents of 55.74%-57.71%, and enrichment in LREE and LILE, and depletion in HREE and HFSE. Apatite belongs to fluoroapatite, and the intercept age (115±4.9 Ma) and weighted mean ²⁰⁶Pb/²³⁸U age (114.7±2.3 Ma) of apatite represent the crystallization age of Huichang pyroxene diorite. While, the zircons have ²⁰⁶Pb/²³⁸U age of 233-271 Ma and ε_Hf(t) value of -3.0 to -1.4, which indicate the captured zircon from Ⅰ-type granite. Combined with the previous regional geological data, the South China block was mainly in a compression environment in the Indosinian, forming a large number of S-type and Ⅰ-type granites. In the Cretaceous, the South China block was mainly in an extensional environment, and multiple stages of mantle-derived magmas underplating events occurred. In the extensional environment, meteoric water and mantle-derived fluids brought sufficient mineralizers such as O₂ and CO₂, which provided important conditions for leaching uranium from source bed and finally forming the uranium deposits.
- U-Pb dating,
- apatite,
- zircon,
- pyroxene diorite,
- southern Jiangxi Province,
- uranium mineralization,
- petrology,
- mineralogy

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References(107)

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