The Qin-Hang Metallogenic Belt (QHMB), an important metallogenic belt in South China, hosts Cu and W–Sn polymetallic deposits. Tongshanling ore field the QHMB is characterized by coexistence of Cu- W-bearing deposits, which are related to granodiorite granite porphyry. This study examined whole-rock geochemistry, geochronology, Sr–Nd–Hf isotopes determine genetic relationship between diverse or...

The Fanchang volcanic basin (FVB) is located in the Middle and Lower Yangtze Metallogenic Belt (MLYMB) between ore districts of Ningwu Tongling. existing deposits FVB are relatively small scale related to late Mesozoic A-type granites. In this paper, crystallization age, major trace element composition, Sr-Nd Hf isotope compositions granites summarized from literature; addition, magnetite H O i...