man’,’serif’" lang=EN-US>///Fluid-sensitive trace element ratios, in shoshonites from Huichang, southern Jiangxi Province, are studied in this paper. Analysis on variations of SiO2 versus K2O, Na2O, FeOT, CaO, MgO and TiO2 shows that the Huichang shoshonite was not formed through crystallization fractionation of a high-K calcalkalic magma. From Ta/Hf-Th/Hf discrimination diagram, it is concluded that it was formed in the intraplate tectonic setting. Combined with Sr-Nd-O-Pb isotopic compositions and Nd isotopic model ages, it is inferred here that the Huaichang shoshonite, was formed by mixing of magmas derived from the enriched paleo-continent (Gondwana?) lithospheric mantle with that from the Mesozoic depleted mantle.