Two types of cumulate gabbros are exposed in Wengeng area, Urad Zhongqi, Inner Mongolia, including olive gabbro and amphibole gabbro. The major petrogenetic minerals in the Beiqigetao gabbros are olive, pyroxene, plagioclase and hornblend. The SHRIMP U-Pb dating from olive gabbro give a concordant age of (269±8) Ma. All the above evidences suggest that olive gabbro and amphibole gabbro were derived from the same mantle sources, which had undergone subduction-related metasomatism except inheriting the mantle source characteristics of the North China Block.