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Hadatu U deposit, Xilingol League (Xilinguole Prefecture), Inner Mongolia, Chinai
| Regional Level Types | |
|---|---|
| Hadatu U deposit | Deposit |
| Xilingol League (Xilinguole Prefecture) | Prefecture |
| Inner Mongolia | Autonomous Region |
| China | Country |
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Latitude & Longitude (WGS84):
43° 9' 59'' North , 112° 21' 59'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Erenhot | 16,427 (2017) | 62.0km |
The ore-bearing horizon of the Hadatu and Barun uranium deposits in the study area is the paleo-valley sand body of the upper member of the Saihan Formation, which is obviously controlled by structure and tectonic evolution. Uranium mineralization has the characteristics of the nearby uranium source. The exposed or hidden medium--acid rock mass around the deposit provides a uranium-rich source for the pre-enrichment and epigenetic mineralization of uranium in the sand body of the ore-bearing horizon.
The upper part of the uranium deposit is mainly composed of mudstone and sandstone, with a thin layer of quaternary sandy soil, gravel layers, and vegetation cover on the surface. The depth of burial for the Hadatu uranium deposit ranges from 260 m to 350 m.
Commodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Rock Types Recorded
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Alphabetical List Tree DiagramList of minerals for each chemical element
Other Regions, Features and Areas containing this locality
Amur PlateTectonic Plate
AsiaContinent
- Gobi DesertDesert
Eurasian Plate
- Erdaojing subduction complexOphiolite Complex
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References
[1]Shi, Liancheng; Li, Huaiyuan; Wang, Nanping; Han, Penghui; Shen, Zhengxin; Yu, Cong; Zhang, Xiang; Meng, Xiangbao (2025) Methods for Verifying the Relationship Between Weak Uranium Anomaly and Uranium-Rich Geological Bodies in the Covered Areas of the Erlian Basin, Inner Mongolia. Minerals, 15 (10). doi:10.3390/min15101013
