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《Acta Geoscientica Sinica》 2012-04
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Genetic Mineralogy of Andalusite in Xiongcun Porphyry Copper-Gold Oredeposit,Tibet

HUANG Yong 1,2),DING Jun 2),TANG Ju-xing 3),ZHANG Li 2),LANG Xing-hai 1) 1) Chengdu University of Technology,Chengdu,Sichuan 610059;2) Chengdu Center of China Geological Survey,Chengdu,Sichuan 610081;3) MLR Key Laboratory of Metallogeny and Mineral Resource Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037  
There are abundant andalusites in the Xiongcun porphyry copper-gold deposit.Three major assemblages are recognized,i.e.,quartz-K-feldspar-muscovite/sericite-andalusite assemblage,andalusite-quartz-sericite/muscovite assemblage,and quartz andalusite sulfide veins.The mineral association,texture and composition of andalusites indicate that the andalusites are of hydrothermal type.The quartz-K-feldspar-muscovite/sericite-andalusite assemblage in early K-silicate alteration zone was formed under the conditions of fairly high temperatures(above 550℃) and relatively low + K/+ H ratios.Early K-silicate alteration was replaced by later phyllic/sericitic alteration under lower P-T and higher + K/+ H conditions,and meteoric water probably entered the collapsed hydrothermal system during this period.Quartz-andalusite-sulfide veins with sericite alteration envelope occur rather rarely and are only observed within the phyllic alteration zone.This assemblage was formed under lower P-T and higher + K/+ H condition.Andalusite assemblages are similar to the El Salvador porphyry copper deposit in Chile.Volcanic tuff and porphyry stock had rich Al 2 O 3,which was favorable for the formation of andalusite.The andalusite within different assemblages helps reconstruct the P-T condition of the magmatic-hydrothermal process.
【Fund】: 自然科学基金(编号:41172077);; 国家973项目(编号:2011CB403103);; 青藏专项(编号:1212010012005);; 西藏大型矿床成矿专属性研究(编号:1212011221073)联合资助
【CateGory Index】: P578.945
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