松辽盆地铁法地区砂岩型铀矿关键控矿因素的时空耦合

彭虎; 焦养泉; 荣辉; 逄礴; 吕东霖; 郭晓丹; 王庆双; 宇文晓依

doi:10.3799/dqkx.2023.073

Volume 49 Issue 9

Sep. 2024

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Article Navigation > Earth Science > 2024 > 49(9): 3182-3198

Peng Hu, Jiao Yangquan, Rong Hui, Pang Bo, Lü Donglin, Guo Xiaodan, Wang Qingshuang, Yuwen Xiaoyi, 2024. Spatial-Temporal Coupling of Key Ore-Controlling Factors for Sandstone-Type Uranium Deposits in Tiefa Area, Songliao Basin. Earth Science, 49(9): 3182-3198. doi: 10.3799/dqkx.2023.073

Citation:

Peng Hu, Jiao Yangquan, Rong Hui, Pang Bo, Lü Donglin, Guo Xiaodan, Wang Qingshuang, Yuwen Xiaoyi, 2024. Spatial-Temporal Coupling of Key Ore-Controlling Factors for Sandstone-Type Uranium Deposits in Tiefa Area, Songliao Basin. Earth Science, 49(9): 3182-3198. doi: 10.3799/dqkx.2023.073

Citation:

Peng Hu, Jiao Yangquan, Rong Hui, Pang Bo, Lü Donglin, Guo Xiaodan, Wang Qingshuang, Yuwen Xiaoyi, 2024. Spatial-Temporal Coupling of Key Ore-Controlling Factors for Sandstone-Type Uranium Deposits in Tiefa Area, Songliao Basin. Earth Science, 49(9): 3182-3198. doi: 10.3799/dqkx.2023.073

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Spatial-Temporal Coupling of Key Ore-Controlling Factors for Sandstone-Type Uranium Deposits in Tiefa Area, Songliao Basin

doi: 10.3799/dqkx.2023.073

Peng Hu^{1, 2, 3
,
,},
Jiao Yangquan^{1, 4
,
,
,},
Rong Hui^{1, 4},
Pang Bo⁵,
Lü Donglin³,
Guo Xiaodan³,
Wang Qingshuang⁶,
Yuwen Xiaoyi⁷

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Institute of Unconventional Oil and Gas, Northeast Petroleum University, Daqing 163318, China
3.
Liaoning Province Geology and Minerals Group Energy Geology Co., Ltd., Shenyang 110013, China
4.
Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China
5.
Liaoning Geological Exploration and Mining Group, Shenyang 110032, China
6.
Shenyang Center of China Geological Survey, Shenyang 110034, China
7.
Liaoning Nuclear Industry Geology 242 Co., Ltd., Xingcheng 125100, China

Received Date: 2022-09-28
Available Online: 2024-10-16
Publish Date: 2024-09-25

Abstract

Abstract

A new uranium deposit and many uranium mineralization spots have been discovered in the Cretaceous strata of the Tiefa area in the southeastern Songliao basin. Based on the regional geological background investigation and the analysis of more than 1 000 drilling data, the author conducts a quantitative and systematic study on the key ore-controlling factors, such as uranium reservoir, interlayer oxidation zone and reducing medium in the uranium metallogenic system from source to sink in the study area. The sandstone-type uranium deposits in the study area have experienced two important stages: the pre-enrichment stage in the depositional stage and the main metallogenic stage in the interlayer oxidation stage. The basin-mountain coupling driven by regional tectonic evolution not only controls the formation and migration of uranium sources, but also drives the tectonic inversion between the two metallogenic stages. The distribution law of uranium mineralization in the study area has obvious spatial coupling relationship with ore control factors such as uranium reservoir heterogeneity, oxidized sand body size, and reducing medium, etc. The gray mudstone at the bottom of the 3rd member of Quantou Formation and the coal seam at the top of the Fuxin Formation restrict the scale of the interlayer oxidation zone and the distribution of uranium mineralization. The 3rd member of Quantou Formation has developed uranium reservoir sand bodies with a complete "mud-sand-mud" structure and obvious clues of uranium mineralization. It is the most favorable layer for sandstone-type uranium mineralization in this area, followed by the glutenite at the bottom of the Fuxin Formation in the western margin of the depression. The most favorable parts for sandstone-type uranium mineralization is in the west of the depression, where the sandstone body of uranium reservoir in the 3rd member of Quantou Formation has changed from thick to thin, the sand content has changed from high to low, the ratio of the thickness to the oxidized sand body decreased, and the external reducing geological bodies such as gray mudstone and coal seams have changed from thin to thick.
- sandstone-type uranium deposit,
- Songliao basin,
- 3rd member of Quantou Formation,
- uranium reservoir,
- ore-controlling factors,
- sedimentology,
- ore deposits

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References(66)

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Spatial-Temporal Coupling of Key Ore-Controlling Factors for Sandstone-Type Uranium Deposits in Tiefa Area, Songliao Basin

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