SEDEX type stratabound and stratiform Pb-Zn deposits, hosted in phosphatic dolomite beds of the Upper Sinian Dengying formation. The mineralizations occur within a narrow stratographic interval and can be traced more or less continuously for about 50 km along the northern bank of the Dadu river.
References:
- Lin Fangcheng, and Pan Guitang (2006): Discovery of seismites in Upper Sinian stratiform lead-zinc deposits in Dadu River valley, Sichuan, China: Implication for ore genesis. Science in China, Series D (Earth Sciences), 49(11), 1135-1146.
Mineral list contains entries from the region specified including sub-localitiesMineral List:10 entries listed. 6 valid minerals.
Localities in this Region: | China | |
- Dadu river valley Pb-Zn mining district
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