Despite numerous studies, the origin of intraplate basalts from eastern Asia is still elusive. This includes the relative importance of subducted oceanic crust and metasomatized lithospheric mantle in generation of these lavas. To address this important issue, we have carried out an integrated Mg-Sr-Nd isotope study of Jiaohe garnet pyroxenite xenoliths and Cenozoic basalts from the Changbaishan-baoqing volcanic belt (CVB), NE China. The Jiaohe garnet pyroxenite xenoliths exhibit low Hf/Hf* ((Hf-N/(Sm-N x Nd-N)(0.5), 0.7-0.9), depleted Sr-Nd isotopic compositions (Sr-87/Sr-86(i) = 0.7035-0.7041; epsilon(Nd) = +2.9 - +8.6) and low delta Mg-26 (-0.61 to -0.39 parts per thousand). These features reflect both protolith heterogeneity and the effect of isotopic exchange with carbonates during subduction. The CVB basalts display variable Mg isotopic compositions. Low-Si basalts are characterized by low delta Mg-26 (-0.27 to -0.44 parts per thousand), variable Hf/Hf* (0.7-1.4) and depleted Sr-Nd isotopic compositions (Sr-87/Sr-86(i) = 0.7039-0.7050; epsilon(Nd) = +1.0 - +4.7), which were attributed to partial melting of upwelling asthenospheric mantle containing recycled oceanic crustal components. In contrast, high-Si basalts display low Hf/Hf* (0.6-0.9), EM1-like Sr-Nd isotopic compositions (Sr-87/Sr-86(i) = 0.7047-0.7054; epsilon(Nd) = -2.4 - -0.2) and normal mantle-like delta Mg-26 values (-0.18 to -0.33 parts per thousand). Such features can be explained by participation of metasomatized lithospheric mantle in their source. The transition from low-Si melts with low-delta Mg-26 to high-Si melts with normal mantle-like delta Mg-26 for the CVB basalts are genetically related to continental rifting, asthenospheric mantle upwelling and mechanical-chemical erosion of basal metasomatized lithosphere induced by subduction of the Pacific oceanic slab. Recycled oceanic crust and basal lithospheric mantle both played a fundamental role in generation of the intraplate basalts in eastern Asia.