收藏切换
Analysis on the Occurrence Characteristics of Uranium Minerals and Mineralization Conditions in the Yimin Formation of Kelulun Depression, Hailar Basin
收藏切换
Fanmin MENG1, Fengjun NIE1, *, Fei XIA1, Zhaobin YAN1, Da SUN1, Wenbo ZHOU2, Rong ZHANG2, Changhong WANG2
Northwestern Geology | 2026, 59(3) : 264 - 278
Less
收藏切换
Northwestern Geology | 2026, 59(3): 264-278
Analysis on the Occurrence Characteristics of Uranium Minerals and Mineralization Conditions in the Yimin Formation of Kelulun Depression, Hailar Basin
Full
Fanmin MENG1, Fengjun NIE1, *, Fei XIA1, Zhaobin YAN1, Da SUN1, Wenbo ZHOU2, Rong ZHANG2, Changhong WANG2
Affiliations
  • 1College of Earth Sciences, East China University of Technology, Nanchang 330013, Jiangxi, China
  • 2Geological Party No. 243, CNNC, Chifeng 024000, Inner Mongolia, China
Published: 2026-06-20 doi: 10.12401/j.nwg.2025040
Outline
收藏切换

The sandstone-type uranium deposit in the Kelulun Depression is the first industrial uranium deposit discovered in the Hailar Basin. In order to preliminarily identify the types, occurrence characteristics, and mineralization significance of uranium minerals in the study area, this paper conducts a systematic study of the ore-bearing sandstone in the target layer by using polarized light microscopy combined with electron probe analysis on the basis of a field investigation. The results show that uranium mineralization in the study area occurs at the front edge of the braided river delta of the Yimin Formation. The rock type of the ore-bearing target layer is mainly medium-fine-grained feldspathic litharenite, with the overall development post-generation alteration. Uranium minerals are mainly coffinite, followed by uranium-titanium oxide. Coffinite is mainly distributed in colloidal or stellate forms in or around pyrite, and a few are filled in the edges of debris particles or dissolution pits in irregular granular form. Uranium-titanium oxides are mostly distributed in irregular granular forms in the biotite cleavage cracks. The coffinite and uranium-titanium oxide, as the first discovered independent uranium minerals in the study area, fill the gap left by the absence of uranium minerals in the Hailar Basin. In terms of uranium mineralization conditions, the Permian granite and intermediate-acidic volcanic rocks in the west of the study area provide sufficient uranium sources for the sandstone-type uranium mineralization in the area. Under the action of reducing media such as oil and gas, organic carbon, and sulfides in the area, U6+ in the ore-forming fluid is reduced to U4+ and precipitated into mineralization in the form of coffinite and uranium-titanium oxide.

sandstone-type uranium deposit  /  coffinite  /  U-Ti oxide  /  Yimin Formation  /  Kelulun Depression
孟繁敏, 聂逢君, 夏菲, 严兆彬, 孙达, 周文博, 张荣, 王长虹. 海拉尔盆地克鲁伦凹陷伊敏组铀矿物赋存特征及铀成矿条件分析. 西北地质, 2026 , 59 (3) : 264 -278 . DOI: 10.12401/j.nwg.2025040
Fanmin MENG, Fengjun NIE, Fei XIA, Zhaobin YAN, Da SUN, Wenbo ZHOU, Rong ZHANG, Changhong WANG. Analysis on the Occurrence Characteristics of Uranium Minerals and Mineralization Conditions in the Yimin Formation of Kelulun Depression, Hailar Basin[J]. Northwestern Geology, 2026 , 59 (3) : 264 -278 . DOI: 10.12401/j.nwg.2025040
Year 2026 volume 59 Issue 3
149
70
Cite this Article
BibTeX
Article Info
doi: 10.12401/j.nwg.2025040
  • Receive Date:2023-04-20
  • Online Date:2026-09-16
  • Published:2026-06-20
Article Data
Affiliations
History
  • Received:2023-04-20
  • Revised:2025-01-12
  • Accepted:2025-03-21
Affiliations
    1College of Earth Sciences, East China University of Technology, Nanchang 330013, Jiangxi, China
    2Geological Party No. 243, CNNC, Chifeng 024000, Inner Mongolia, China
References
Share
https://castjournals.cast.org.cn/joweb/xbdz/EN/10.12401/j.nwg.2025040
Share to
QR

Scan QR to access full text

Cite this article
BibTeX
Citations
表12种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
关闭全屏
  • BibTeX
  • EndNote
  • RefWorks
  • TxT