Based on detailed studies of petrographic characteristics and major elements of minerals, the authors analyzed trace elements of Cpx in the peridotitic xenoliths from Jining area, Inner Mongolia. The relationship between the Ol-Mg and the equilibrium temperature of the peridotites suggests the coexistence of fertile mantle and refractory-transitional mantle beneath the study area in Cenozoic period. Such phenomena might be attributed to the reformation of the cratonic SCLM by the upwelling asthenospheric materials and the eventual replacement resulting from the cooling of the upwelled asthenosphere under heterogeneous conditions.