Isotope constraints on hydrothermal fluids in massive sulfide deposits
Stable and radiogenic isotope techniques are powerful tools to trace the origin and evolution of hydrothermal ore-forming fluids associated with massive sulfide deposits. In this paper, endeavors are summarized to use H, O, C, S, B, Si, Cu, Pb, Sr, Nd, Os, and He isotopes in the study of a number of Chinese massive sulfide deposits and the Sullivan deposit in Canada. Direct dating of these massive sulfide deposits is also critical for properly evaluating their origin and distinguishing multiple hydrothermal events, and promising results are obtained by using various methods such as Pb-Pb, Rb-Sr, Sm-Nd, and Re-Os isotopes.
S.Y.Jiang
State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences,Nanjing University, Nanjing, China
国际会议
第十二届水-岩相互作用国际研讨会(P0roceedings of the 12th International Symposium on Water-Rock Interaction)
昆明
英文
13-16
2007-07-31（万方平台首次上网日期，不代表论文的发表时间）