Hydrothermal lead-zinc deposit, hosted by Devonian limestone, sandstone and shale that are locally intruded by granites and some lamprophyre dikes. The deposit straddles the border between Gongcheng and Yangshuo counties and is jointly worked by the Daoping and Yangshuo mines which are connected underground.
Ref.:
- Guanghua Liu and Ottens, B. (2005): Daoping Mine, Guangxi, China. The Mineralogical Record 36(1) 25-33.
