Title: Geological features and prospecting direction of the Camelfield gold deposit,Inner Mongolia
Abstract: 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 midsouth of Daxinganling.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,its 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 526×10-6~1248×10-6,the associated Ag is 2898×10-6~8090×10-6 and Cu is 050%~331%. The metallogenic type is magmatic hydrothermal fillreplacementing type gold deposit that related to medium ultrabasic invade rock.
Publication Year: 2003
Publication Date: 2003-01-01
Language: en
Type: article
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