作者: Lijuan Wang , Yuwang Wang , Jingbin Wang , D. Günther
DOI: 10.1007/S11434-006-2163-4
关键词:
摘要: LA-ICP-MS analyses on single fluid inclusions trapped in fluorite and quartz from the Sn-Cu orebody of Dajing deposit Sn Huanggangliang were conducted to trace source evolution Cu-rich Sn-rich fluids using Rb/Sr Sn/Cu ratios fluids. The results show that deposit, relatively rich Na probably derived deep-seated basic magma, contain Cu several tens times more than Sn, Sr Rb, while fluids, K high level granitic Cu, Rb Sr. It is suggested mixed at stage moderate low temperature salinity, resulting formation Cu-Sn orebodies central part deposit.