Abstract: According to the survey and analysis of trace elements in Donggangling limestone of Fengcun lead-zinc mine，the results show: Mn content ranges from 208.3×10^-6 to 3 191×10^-6，with the average Mn content of 1 027.42×10^-6;Sr content ranges from 28.69×10^-6 to 488.9×10^-6，with the average Sr content of 300.45×10^-6.w(Sr) /w (Ba)>1，it may be the normal marine sediments.And，w(Sr)/w(Cu) is generally greater than 10，indicating that the sedimentary of limestone is in a closed，dry，anoxic reduction environment.The Pb，Zn contents are significantly higher than the crustal abundance.It is inferred that Donggangling limestone is the main source of the ore.Besides，based on the w（U）/w（Th）>1 in some ore samples，it indicates that Fengcun lead-zinc deposit has the characteristics of sedimentary superimposed hydrothermal reformation type deposit，resulting from the hydrothermal reformation at latter period.

Key words: Fengcun lead-zinc deposits, Donggangling limestone, Trace element, Sedimentary environment, Hydrothermal reformation