Geological features and prospecting direction of the Camelfield gold deposit,Inner Mongolia

The Camelfield gold deposit occurs in the east of Huanggangliang to Ganzhuermiao mineralization belt,and is the only deposit which dominated by gold,but associates Ag,Cu in the midsouth of Daxinganling.There are 3 industrial orebodies has been outlined in the area,the orebodies occur in the dioritebody of Indosinian and controlled by NWW fault structures,its altered rock type gold deposit occurs in fracture zones.Alteration includes silicification,sericitization,chloritization,epidotization,kaolintization and carbonatization, metal mineralization includes pyritization,chalcopyritization,magnetitization,bornitization,limonitization and malachitization. The average grade of gold is 526×10-6～1248×10-6,the associated Ag is 2898×10-6～8090×10-6 and Cu is 050%～331%. The metallogenic type is magmatic hydrothermal fillreplacementing type gold deposit that related to medium ultrabasic invade rock.