Widespread Cenozoic intraplate basalts from eastern China offer the opportunity to investigate the consequences of interaction between the stagnant Pacific slab and overlying asthenosphere and chemical heterogeneity within this “big mantle wedge”. We present and compile a comprehensive study of highly siderophile elements and Mg-Zn isotopes of this magmatic suite (60 samples including nephelinites, basanites, alkali basalts and tholeiites). The large-scale Mg-Zn isotopic anomalies documented in these basalts have been ascribed to mantle hybridization by recycled Mg-carbonates from the stagnant western Pacific plate. Our results reveal that the nephelinites and basanites are characterized by unfractionated platinum-group element (PGE) patterns normalized to primitive upper mantle (PUM) (e.g., Pd_N/Ir_N normalized to PUM = 1.1 ± 0.8, 1σ), relatively high total PGE contents (e.g., Ir = 0.25 ± 0.14 ppb) and modern mantle-like ¹⁸⁷Os/¹⁸⁸Os (0.142 ± 0.020). These characteristics are coupled with lighter Mg isotope (δ²⁶Mg = −0.48 ± 0.07‰) and heavier Zn isotope (δ⁶⁶Zn = +0.46 ± 0.06‰) compositions compared to the mantle values (δ²⁶Mg: −0.25 ± 0.07‰; δ⁶⁶Zn: +0.18 ± 0.05‰). Together, these data are interpreted to reflect the oxidative breakdown of low proportions of mantle sulfides in the sources of these small-degree melts, likely caused by recycled carbonates, which then release chalcophile-siderophile elements into carbonatitic melts. By contrast, the contemporaneous alkali basalts and tholeiites are characterized by highly fractionated PGE patterns (e.g., Pd_N/Ir_N = 4.4 ± 3.3; Ir = 0.037 ± 0.027 ppb) and radiogenic ¹⁸⁷Os/¹⁸⁸Os (0.279 ± 0.115) coupled with less fractionated Mg-Zn isotope compositions (δ²⁶Mg: −0.39 ± 0.05‰; δ⁶⁶Zn: +0.35 ± 0.03‰). In combination with other isotopic (e.g., Sr-Nd) and chemical (SiO₂, Ce/Pb, Ba/Th, Fe/Mn) constraints, the alkali basalts and tholeiites were derived from higher degree melting of ancient pyroxenite-bearing mantle in addition to mixing with the aforementioned nephelinitic and basanitic melts. Collectively, we suggest that deep recycled carbonates promoted melting within the “big mantle wedge” leading to the generation of Cenozoic intraplate basalts across eastern China and the “redox freezing of carbonates” may cause the oxidation of Fe⁰ and S^2-. This process may provide an important mechanism to oxidize mantle sulfides and transfer precious metals from deep mantle to crust.