Perigranitic vein-type uranium deposit, hosted in Upper Sinian and Lower Cambrian metasediments between the Xuehuading and Jinjiling granitic massifs in the west and east, respectively. The area belongs to the Jiuyishan-Jinjiling granite complex, which forms part of the Nanling granite belt.
References:
- Dahlkamp, F.J., Ed. (2009): Uranium Deposits of the World. Springer (Berlin, Heidelberg), pp. 31-156.
Mineral List:7 entries listed. 6 valid minerals.
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