Medium-scale epitermal Au-Ag-Mn vein deposit, hosted in Late Jurassic felsic pyroclastics rocks of the Zhangjiakou Formation, that are intruded by several small granite porphyritic stocks to which the deposit is related. The veins are controlled by NNW-trending faults and have a strike length of 1200 m.
Ref.:
- Guo Guangjun and Wang Shiqi (1998): REE Geochemistry of Xiaokouhuaying Silver-Manganese Deposit in Hebei Province. Acta Scientiarium Naturalium Universitatis Pekinensis 34(4), 510-518.
-
http://wrgis.wr.usgs.gov/open-file/of03-220/DATABASE/lode_deposits.txt
6 entries listed. 6 valid minerals.