Lead isotopic compositions of 29 Tertiary basalts in the Jiyang depressional basin are reported in this paper. It is indicated that lead isotopic compositions of these basalts vary obviously. Their 206Pb/204Pb ratios are 16. 864 -18. 361, 207Pb/204Pb, 15. 268-15. 599 and 208Pb/204Pb, 36. 770-39. 118. On the 20SPb/204Pb-2<)6Pb/204Pb diagram, the Tertiary basalts are ploted above NHRL line and their A8/4 values are all larger than 60, suggest-ing the occurrence of Dupal anomaly in their mantle source. On the Pb-Pb and Pb-Sr correlation diagrams, all data points have a good linear relation indicating the binary mixing characteristics and are all located between the endmember components of DMM, EM I and EM I . Because the positive Nb anomaly and higher MgO con-tents and Mg# number values of these basalts, it is not important that the crustal contamination occurred during the ascending process of basaltic magma. Therefore, we conclude that the obvious variations of Pb isotopic com-position are mainly attributed to the mixing process of different degree between the different endmember compo-nents during the formation of basaltic magma.