Alkali granites are exposed in Jingesitai area near China-Mongolia border area.The intrusions, which were assigned to Late Hercynian or Indosinian in 1:200 000 regional geological survey, constitute a part of the southern belt alkali granites in the Xingmeng orogenic belt.Alkali granites are characterized by high silica, high alkali, quasi-aluminum and low magnesium and calcium.The content of silica varies from 74.80% to 78.74%, that of K2O is higher than that of Na2O, and that of alkali is higher than 8%.The REE content is low, the fractionation between LREE and HREE is not very obvious, (La/Yb)N values vary from 0.898 to 5.168 and δEu values are in the range of 0.07~0.89.Therefore, the granites belong to PAG and might have been the product of post-orogeny.U-Pb isotopic age dating of the alkali granite is (284.8±1.1) Ma, implying a product of Early Permian magmatism.