粤北长江铀矿田辉长闪长岩的岩石成因及其与铀成矿的关系

钟福军; 潘家永; 巫建华; 夏菲; 伏顺成; 祁家明; 赵奇峰

doi:10.3799/dqkx.2017.592

Volume 44 Issue 9

Sep. 2019

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Article Navigation > Earth Science > 2019 > 44(9): 3042-3059

Zhong Fujun, Pan Jiayong, Wu Jianhua, Xia Fei, Fu Shuncheng, Qi Jiaming, Zhao Qifeng, 2019. Petrogenesis and Its Relationship with Uranium Mineralization of Gabbro-Diorite in Changjiang Uranium Ore-Field, Northern Guangdong Province, China. Earth Science, 44(9): 3042-3059. doi: 10.3799/dqkx.2017.592

Citation:

Zhong Fujun, Pan Jiayong, Wu Jianhua, Xia Fei, Fu Shuncheng, Qi Jiaming, Zhao Qifeng, 2019. Petrogenesis and Its Relationship with Uranium Mineralization of Gabbro-Diorite in Changjiang Uranium Ore-Field, Northern Guangdong Province, China. Earth Science, 44(9): 3042-3059. doi: 10.3799/dqkx.2017.592

Citation:

Zhong Fujun, Pan Jiayong, Wu Jianhua, Xia Fei, Fu Shuncheng, Qi Jiaming, Zhao Qifeng, 2019. Petrogenesis and Its Relationship with Uranium Mineralization of Gabbro-Diorite in Changjiang Uranium Ore-Field, Northern Guangdong Province, China. Earth Science, 44(9): 3042-3059. doi: 10.3799/dqkx.2017.592

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Petrogenesis and Its Relationship with Uranium Mineralization of Gabbro-Diorite in Changjiang Uranium Ore-Field, Northern Guangdong Province, China

doi: 10.3799/dqkx.2017.592

1.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
2.
Research Institute No. 290, CNNC, Shaoguan 512026, China
3.
Research Institute No. 270, CNNC, Nanchang 330013, China

Received Date: 2017-06-05
Publish Date: 2019-09-15

Abstract

Abstract

Understanding for uranium mineralization was absolutely restricted by the petrogenesis of gabbro-diorite,which emplaced into the Yanshanian biotite granite at the deep part of Changjiang uranium ore-field. We provide LA-ICP-MS zircon UPb age,Lu-Hf isotopic,mineralogical and geochemical evidence to analyse the poetrogenesis,tectonic background and its relationship with uranium mineralization. Gabbro-diorite emplaced at the Late Jurassic (LA-ICP-MS zircon U-Pb isotopic age:150±1 Ma (n=17,MSWD=0.18)) and was geochemically characteristic of within-plate basalt. The magma evolution process (ranges from basic to neutral magma) has been effectively recorded by the transformation of major elements in zoned plagioclase and biotite from gabbro-diorite. The zircon ε_Hf(t) values range from -14.1 to -8.6 and the two-stage model ages (t_DM2) range from 1.7 Ga to 2.1 Ga. The magmatic source was the relatively enriched mantle changed by the metasomatism fluid originated from the subduction zone of Pacific Ocean Plate which started from the Middle Jurassic. Gabbro-diorite has undergone a variational degree crustal contamination with the Proterozoic-Palaoproterozoic crustal material in the process of emplacement during the Late Mesozoic large scale lithosphere thining tectonic background. Gabbro-diorite provides a better reductive environment than the granite for uranium mineralization,prompting U⁶⁺ been reduced to pitchblende in the ore forming hydrothermal fluid.
- gabbro-diorite,
- lithospheric thining,
- uranium mineralization,
- intersection type uranium,
- Changjiang uranium ore-field,
- geochronology

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References(101)

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Petrogenesis and Its Relationship with Uranium Mineralization of Gabbro-Diorite in Changjiang Uranium Ore-Field, Northern Guangdong Province, China

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