Metallogenic Conditions and Genesis of the Shangjiaoshan Gold Deposit in Du'an,Debao County,Guangxi
Zhou Fan
Abstract
Zhou Fan
Abstract
The Sanjiaoshan gold deposit occurs mainly in the clasolite and pelitic siltstone in Tangding group in lower Devonian system which strictly controlled by strata,faults and folds.The types of ore are mainly argillaceous,and silica oxidized ores in less.The host rocks are pelite argillaceous siltite and sillcalite.The alterations of the host rock include silicification,limonitization and argillation.With field reconnaissance geological survey,this paper figures out good mineralization for gold mine in this area,and analyses the genesis of this gold deposit based on the information from former researchers,and suggests that this deposit belongs to Carlin type gold deposit,that's a minute dissemination medium-low hydrothermal deposit with atmospheric water filtering genesis.
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The Sanjiaoshan gold deposit occurs mainly in the clasolite and pelitic siltstone in Tangding group in lower Devonian system which strictly controlled by strata,faults and folds.The types of ore are mainly argillaceous,and silica oxidized ores in less.The host rocks are pelite argillaceous siltite and sillcalite.The alterations of the host rock include silicification,limonitization and argillation.With field reconnaissance geological survey,this paper figures out good mineralization for gold mine in this area,and analyses the genesis of this gold deposit based on the information from former researchers,and suggests that this deposit belongs to Carlin type gold deposit,that's a minute dissemination medium-low hydrothermal deposit with atmospheric water filtering genesis.
Key concepts: Pelite, Geology, Siltstone, Devonian, Geochemistry, Mineralization (soil science), Hydrothermal circulation, Mining engineering