Magmatic evolution and related W–Mo mineralization in the Larong deposit, eastern Tibet: Evidence from zircon U–Pb ages, geochemistry and Sr–Nd–Hf isotopes

The Late Cretaceous (ca. 92 Ma) Larong porphyry W–Mo deposit (39.44 Mt WO3 @ 0.1541%) is the first-discovered giant W–Mo deposit in the Leiwuqi-Zogang metallogenic belt, Sanjiang region. Multi-stage granitoids including the dacite porphyry (DP), granodiorite porphyry (GP), biotite granite porphyry (BGP), monzogranite porphyry (MP), biotite granite (BG), and granite aplite (GA) have been identified in the Larong deposit. However, the magmatic...