松辽盆地钱家店铀矿床层间氧化带结构定量表征及制约因素

曹民强; 荣辉; 陈振岩; 焦养泉; 里宏亮; 王岩; 李青春

doi:10.3799/dqkx.2020.375

Volume 46 Issue 10

Nov. 2021

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Article Navigation > Earth Science > 2021 > 46(10): 3453-3466

Cao Minqiang, Rong Hui, Chen Zhenyan, Jiao Yangquan, Li Hongliang, Wang Yan, Li Qingchun, 2021. Quantitative Characterization and Controlling Factors of the Interlayer Oxidation Zone of Qianjiadian Uranium Deposit, Songliao Basin. Earth Science, 46(10): 3453-3466. doi: 10.3799/dqkx.2020.375

Citation:

Cao Minqiang, Rong Hui, Chen Zhenyan, Jiao Yangquan, Li Hongliang, Wang Yan, Li Qingchun, 2021. Quantitative Characterization and Controlling Factors of the Interlayer Oxidation Zone of Qianjiadian Uranium Deposit, Songliao Basin. Earth Science, 46(10): 3453-3466. doi: 10.3799/dqkx.2020.375

Citation:

Cao Minqiang, Rong Hui, Chen Zhenyan, Jiao Yangquan, Li Hongliang, Wang Yan, Li Qingchun, 2021. Quantitative Characterization and Controlling Factors of the Interlayer Oxidation Zone of Qianjiadian Uranium Deposit, Songliao Basin. Earth Science, 46(10): 3453-3466. doi: 10.3799/dqkx.2020.375

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Quantitative Characterization and Controlling Factors of the Interlayer Oxidation Zone of Qianjiadian Uranium Deposit, Songliao Basin

doi: 10.3799/dqkx.2020.375

1.
Development Company of New Energy Sources of Liaohe Petroleum Exploration Bureau, Panjin 124010, China
2.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China

Received Date: 2020-06-22
Available Online: 2021-11-03
Publish Date: 2021-11-03

Abstract

Abstract

Quantitative characterization of architecture of the interlayer oxidation zone is very important to reveal the regularity of uranium mineralization. In this study, the interlayer oxidation zone of the Qianjiadian uranium deposits in the Songliao basin was quantitatively characterized by sedimentological and geochemistry mappings. It is found that the interlayer oxidation zone of the deposit is mainly composed of red sandstone, light yellow sandstone, gray white sandstone, gray mineralized sandstone and primary gray sandstone, respectively corresponding to strong oxidised subzone, weak oxidised subzone, faint oxidised subzone, transitional zone and reduction zone. The uranium mineralization is closely related to the internal architecture of interlayer oxidation zone. The main industrial uranium ore bodies are strictly developed in the transitional zone. A few ore bodies whose continuity is poor occur in the faint oxidised subzone. The ore bodies are sporadically distributed in the weak oxidation subzone. The low-grade uranium ore bodies are found in the side of reduction zone close to transitional zone. Formation of the interlayer oxidation zone is restricted by the heterogeneity of uranium reservoir sandstones and depositional systems. The oxidised zone is mainly developed in sand bodies of the braided river and braided distributary channel, and the transition zone primarily distributed at the edge of the braided distributary channel or in the crevasse fan.
- interlayer oxidation zone,
- sandstone-type uranium deposit,
- Qianjiadian uranium deposit,
- Songliao basin,
- uranium reservoir,
- sedimentology

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