The formation of the Suyunhe large porphyry Mo deposit in the West Junggar terrain, NW China: Zircon U-Pb age, geochemistry and Sr-Nd-Hf isotopic results
文摘
Host rocks are granite, granite porphyry, granodiorite porphyry, and monzonitic granite porphyry. Host rocks emplaced at 298–295 Ma (granite) and 295–294 Ma (granodiorite porphyry). Host rocks originated from the partial melting of juvenile lower crust. Juvenile crust provided Mo which results in the formation of the Suyunhe Mo deposit.