Late Jurassic Sn metallogeny in eastern Guangdong, SE China coast: Evidence from geochronology, geochemistry and Sr-Nd-Hf-S isotopes of the Dadaoshan Sn deposit
The Dadaoshan Sn mineralization and related granite formed at ca. 153 Ma. Late Jurassic Sn mineralization also occurred in the SE China coastal area. The granite is fractionated I-type granite and produced from partial melting of crust. Both the granite and the mineralization formed in an extensional setting.