Re-Os and U-Pb geochronology of the Shazigou Mo polymetallic ore field, Inner Mongolia: Implications for Permian-Triassic mineralization at the northern margin of the North China Craton
The Shazigou Mo–W–Pb–Zn ore field has been discovered recently in Inner Mongolia. The Mo–W–Pb–Zn mineralization in the Shazigou ore field took place at ∼245 Ma. The Mo fluid was derived from magmatic sources with crustal contamination and assimilation. The Pb–Zn fluid was intensely influenced by metamorphic and meteoric waters.