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- W2374089073 abstract "Axi gold deposit and its peripheral ore deposits Yiermande, Qiabukanzuota, which formed in Late Paleozoic volcanic rocks in West Tianshan Mountains, are considered as epithermal mineralizing type,and divided furtherly into adularsericite type and silicated rock type The gold deposits are formed in TulasuYelimodun volcanic belt of Yili Late Paleozoic rift And the country rocks of the gold deposit are continental intermediateacid volcanic eruptive rock series of Dahalajunshan formation(C1d) and corresponding subvolcanic bodies which belong to limealkalialkali series association Axi gold deposit considered as the representative of the adularsericite type was controlled by volcanostructures and the main ore bodies were quartz vein type filling in ringlike fault near craterAnd it is lowtemperature and lowpressure feature by its ore texture and mineral assembladgeYiermande gold deposit considered as the representative of the silicated rock type was controlled by the sedimentary volcanic rocks of the lower part of Dahalajunshan formation and its ore bodies are layer and layerlike So by analyzing the metallogenogeochemical characteristics of the ore deposits,the authors discuss the settings,conditions and the characteristics of the gold deposit and set up its oreforming model with epithermal characteristics" @default.
- W2374089073 created "2016-06-24" @default.
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- W2374089073 date "2003-01-01" @default.
- W2374089073 modified "2023-09-25" @default.
- W2374089073 title "The geochemical characteristics and ore-forming model of the epithermal gold deposit in West Tianshan Mountains" @default.
- W2374089073 hasPublicationYear "2003" @default.
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