Vein-type uranium deposit, hosted in fractured, strongly altered granite in the contact zone between the Daguzhai porphyritic two-mica granite and the Luobuli porphyritic biotite granite, both of which are of Yanshanian age. The deposit was discovered in the early 1960s, and mined from 1963 to 1985.
Ref.:
- Maozhong Min, Changquan Fang, and Mostafa Fayek (2005): Petrography and genetic history of coffinite and uraninite from the Liueryiqi granite-hosted uranium deposit, SE China. Ore Geology Reviews 26(3/4), 187-197.
- Yaohui Jiang, Hongfei Ling, Shaoyong Jiang, Weizhou Shen, Honghai Fan, and Pei Ni (2006): Trace Element and Sr-Nd Isotope Geochemistry of Fluorite from the Xiangshan Uranium Deposit, Southeast China. Economic Geology 101, 1613-1622.
