The Chaobuleng iron deposit is located in the Erlianhaote-Dong Ujimqin Banner polymetallic metallogenic belt of Inner Mongolia. The medium-coarse-grained granite in the area has close genetic relationship with the Chaobuleng skarn iron deposit, and hence was chosen to determine the SHRIMP U-Pb age. The results show that the granite intruded in (136.9±1.5) Ma, which is consistent to the mineralization age of (140.7±1.8) Ma (Re-Os), suggesting that the mineralization and the rock-forming process occurred at the same time. An analysis of regional metallogenic geological setting shows that mineralization of the metallogenic belt might have occurred in Yanshanian period.