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- W2347273616 abstract "Qingshan gold deposit occurred in the hydrothermal basin margin which between the Shangdan suture zone and Mianlue suture zone.The orebodys occur as vein,cystic,lenticular and stratoid bed in the carbonaceous slate and carbonatite,which located above the disconformity between Jiuliping Group and Jiehejie Group.The ores are divided into primary gold bearing pyrite-siderite type and gossan type.The main metallic mineral in the ore are siderite,pyrite,limonite and gold.The element association is Au-Ag-As-Sb-Ba.Hydrogen and isotope values of the ore-forming fluids have the phenomenon of oxygen drift.The metallogenic temperature ranges from 160~220 ℃,the ore-forming fluid is underground thermal brine which is bicarbonate-sodium chloride type.It is suggested that Qingshan gold deposit is hot spring type,which is formed by the Mesozoic chronically repeated recycling in the Devonian System.The underground hot brine became progressively rich in gold and deposited in structure network." @default.
- W2347273616 created "2016-06-24" @default.
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- W2347273616 date "2009-01-01" @default.
- W2347273616 modified "2023-09-24" @default.
- W2347273616 title "Preliminary Study on the Origin and Geochemical Characteristics in the Qingshan Gold Deposit,Shaanxi Province" @default.
- W2347273616 hasPublicationYear "2009" @default.
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