Abstract: The present paper deals, in detail, with the major element, trace element and rare earth element characteristics of the Arenshaobu gabbro masses in the Wurinitu region, northern Inner Mongolia, with the stress on the petrogenesis, origins of the primitive magmas and their geological implications. The Arenshaobu gabbro masses have SiO₂ contents of 49.62%, Al₂O₃ contents of 17.34%, CaO contents of 8.94%, TiO₂ contents of 1.44%, and P₂O₅ contents of 0.26%. The gabbro masses are enriched in LILE, and depleted in HFSE. The higher Mg# values (0.28-0.68, with an average of 0.52) suggest the origin of the mantle-derived primitive basaltic magmas with lower degrees of crystallization and differentiation during the ascending processes of the magmas. The zircon UPb ages are dated at 309±2 Ma, indicating that the crystallization ages of Arenshaobu gabbro masses may be dated back to the Late Cretaceous. The crystallization temperatures are measured at 928℃ for quartz, and 1206℃ for plagioclase. The depths for the magmatic colling and mineral cocrystallization are more than 10 km, and the crystallization of the Arenshaobu gabbro masses occurred in the deeper-seated magma chambers. The continentalmargin arc geochemical signatures of the Arenshaobu gabbro masses have mirrored that the subduction, replacement and enrichment in the mantle source areas might have taken place prior to the formation of the magmas.