四川会理芭蕉箐地区钠长岩地球化学、年代学特征及其意义

刘亚杰; 徐争启; 宋昊; 李涛; 张苏恒; 姚建

doi:10.3799/dqkx.2022.231

Volume 49 Issue 3

Mar. 2024

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Article Navigation > Earth Science > 2024 > 49(3): 893-906

Liu Yajie, Xu Zhengqi, Song Hao, Li Tao, Zhang Suheng, Yao Jian, 2024. Geochemical and Chronological Characteristics and Significance of Albite in Bajiaojing Area, Huili, Sichuan. Earth Science, 49(3): 893-906. doi: 10.3799/dqkx.2022.231

Citation:

Liu Yajie, Xu Zhengqi, Song Hao, Li Tao, Zhang Suheng, Yao Jian, 2024. Geochemical and Chronological Characteristics and Significance of Albite in Bajiaojing Area, Huili, Sichuan. Earth Science, 49(3): 893-906. doi: 10.3799/dqkx.2022.231

Citation:

Liu Yajie, Xu Zhengqi, Song Hao, Li Tao, Zhang Suheng, Yao Jian, 2024. Geochemical and Chronological Characteristics and Significance of Albite in Bajiaojing Area, Huili, Sichuan. Earth Science, 49(3): 893-906. doi: 10.3799/dqkx.2022.231

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Geochemical and Chronological Characteristics and Significance of Albite in Bajiaojing Area, Huili, Sichuan

doi: 10.3799/dqkx.2022.231

Liu Yajie^{1
,
,},
Xu Zhengqi^{1, 2, 3
,
,
,},
Song Hao^{1, 2},
Li Tao¹,
Zhang Suheng¹,
Yao Jian⁴

1.
Applied Nuclear Techniques in Geosciences Key Laboratory of Sichuan Province, Chengdu 610059, China
2.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China
3.
Key Laboratory of Earth Exploration and Information Techniques, Ministry of Education, Chengdu 610059, China
4.
280 Institute of Nuclear Industry, Guanghan 618300, China

Received Date: 2022-03-23
Available Online: 2024-04-12
Publish Date: 2024-03-25

Abstract

Abstract

Located in the middle and southern part of the Kangdian axis, Bajiaojing area in Huili, Sichuan Province is a rare Proterozoic uranium mining area in China. However, the relevant study is insufficient due to its complex structural conditions, and hardly any research has been reported on albite, an important uranium bearing rock in this area, which seriously restricts further uranium exploration. On the basis of previous studies, through the field geological survey of 1841 uranium mineralization points in Bajiaojing area, the geochemical analysis of rock elements of albite and the test analysis of zircon U-Pb chronology, it is found that albite in the study area is divided into magmatic albite and metasomatic albite. The samples are enriched in Th, U, Zr and REE, and relatively depleted in Ba, K, Sr and Rb. The dating results show that the two main peak ages are ~2.3 Ga and ~1.8 Ga. The albite is mainly derived from the partial melting of metamorphic mudstone in the lower crust and the addition of mantle derived materials, which was formed in the tectonic environment of intracontinental rift. The formation of its protolith is related to the collision event in the southwest margin of the Yangtze platform during 2.4-2.3 Ga, and underwent magmatism at about 1.8 Ga to form albite, and U element is enriched here. The two magmatic activities recorded by its chronological data are the response of the convergence of Columbia supercontinent in the southwest margin of the Yangtze block.
- Southwest margin of Yangtze block,
- Columbia supercontinent,
- albite,
- geochemistry,
- zircon U-Pb,
- Pb dating,
- petrology

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References(59)

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Geochemical and Chronological Characteristics and Significance of Albite in Bajiaojing Area, Huili, Sichuan

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