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The Weilasituo and Bairendaba Zn–Pb–Ag–Cu–(Sn–W) sulphide deposits are located in the southern part of Great Xing'an Range of Inner Mongolia in China. The deposits are located at shallow depths in the newly discovered Weilasituo porphyry hosting Sn–W–Rb mineralization. The mineralization at Weilasituo and Bairendaba consist of zoned massive sulphide veins within fractures cutting the Xilinhot Metamorphic...
The Haoyaoerhudong gold deposit is located in the Urad Middle Banner area of Inner Mongolia in China, and is hosted by black schist of the Bilute Formation in the Mesoproterozoic Bayan Obo Group. The gold mineralization is within a 4500m long and 100m wide zone associated with sulphide(–quartz) veins following the schistosity and crosscutting fractures in the host-rocks; locally as disseminated sulphide...
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