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《Acta Geoscientica Sinica》 2012-04
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Hydrothermal Alteration Distribution Model of the Jiama(Gyama) Copper-Polymetallic Deposit Based on Shortwave Technique

GUO Na 1,2),GUO Ke 1,2),ZHANG Ting-ting 3),LIU Ting-han 2),HU Bin 2),WANG Chong-wu 2) 1) Key Lab of Geomathmatics of Sichuan Province,Chengdu,Sichuan 610059;2) Chengdu Technology University,Chengdu,Sichuan 610059;3) Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037  
The Jiama(Gyama) copper-polymetallic ore deposit is a superlarge ore deposit in the eastern part of central Gangdise.The hydrothermal alteration minerals of the ore body mainly include muscovite,chlorite,biotite,anhydrite,kaolinite,dickite,topaz and calcite,as identified by short wave infrared measurement.The muscovite has close relations with copper polymetallic mineralization,and the thickness of the ore body has the positive correlation with the sample number of aluminum-poor muscovite.The distribution trend of biotite represents potassic alteration,which suggests that the heat center of Jiama(Gyama) ore body lies in the north of exploration line ZK2416-ZK3216.Magnesium-rich chlorite is distributed outside of the aluminum-poor muscovite.In addition,magnesium-rich chlorite and aluminum-poor chlorite have the same significance of heat center.The distribution model,short of phengite,shows that the heat center is quite deep in the mining area.Therefore,the Jiama(Gyama) porphyry system with low denudation extent must have high ore potential in its periphery.
【Fund】: 国家973项目(编号:2011CB403103);; 青藏专项(编号:1212010012005);; 中央公益性行业科研专项(编号:200911007-02)联合资助
【CateGory Index】: P618.41;P631.7
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