Geochronology and Petrology of the Beiligaimiao Magmatic Sulfide Deposit in the Northern Margin of North China Craton, Inner Mongolia.

The article focuses on geochronology and petrology of the Beiligaimiao Magmatic Sulfide Deposit in the northern margin of North China Craton in inner Mongolia, and Beiligaimiao magmatic sulfide deposit is hosted in a small ultramafic intrusion which occurs in the southern part of the Central Asian Orogenic Belt (CAOB) in inner Mongolia. It also mentions that the Beiligaimiao ultramafic intrusion is mainly composed of lherzolite.