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《Geological Science and Technology Information》 2006-01
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Dynamics of Magma Evolvement of Atishi Granite Body in Nurt Area,Xinjiang

YUAN Feng,ZHOU Tao-fa,TAN Lu-gui,FAN Yu,YUE Shu-cang(School of Resources and Environmental Engineering,Hefei University ofTechnology,Hefei 230009,China)  
The Nurt area is located in the north of Altay,Xinjiang,where the granites are widely exposed.The intrusion is adamellite and belongs to high kalium cal-alkaline series with peraluminous characteristics,showing an osculating relationship with the Aketisikan gold deposit.The paper studies the evolvement of magma of Atishi intrusion formed at Yanshanian stage through dymamics of magma and calculated the dynamics parameters,including viscosity,density and Raileigh.The Raileigh value is higher than 10~4,indicating the existence of convection of magma.The simulation shows that the segregation separation of the big relicts is obvious,and that of the small relicts is little.The crystals distribution parameter S values range from 10~(-3) to 10~(-7),indicating that the crystals were floating in magma and controlled by the movement of liquid.The stereology characteristics of plagioclase indicate that the component of magma changed through differential movement between crystal and melted with convective condition.
【Fund】: 国家重点基础研究发展规划项目(2001CB4098);; 安徽省优秀青年科技基金资助项目(04045063);; “九五”国家科技攻关项目(96-915-02-04 新疆305)
【CateGory Index】: P588.11
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