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《Geology in China》 2008-06
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Discovery and significance of scheelite orebodies in the Zhaishang gold deposit,southern Gansu

LIU Jia-jun1,2,LIU Guang-zhi3,LIAO Yan-fu3,ZHENG Wei-jun3,YUE Lian-xiong3,HUA Shu-guang3,MAO Guang-jian1,2,WU Sheng-hua1,2(1.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China;2.Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education,China University of Geosciences,Beijing 100083,China;3.No.5 Gold Geological Party of Chinese Armed Police Force,Xi'an 710100,Shanxi,China)  
Located in the western part of the Min-Li metallogenetic belt,wetern Qinling Mountains,the Zhaishang gold deposit is a recently discovered large Carlin-type disseminated gold deposit.Examination of ores by optical microscope,EPMA and ICP-MS from the the deposit,has revealed a scheelite enrichment.On the basis of chemical-analytical data,several independent scheelite orebodies are located.It belong to Au-Sb-W deposit association of gold-scheelite-stibnite.In some ways,it can be compared with the Manaoke gold deposit in Sichuan with respect to geological setting,host lithology,mineralization style,mineral assemblages,geochemical association and metallogenic processes involved.Since in the Devonian and Triassic strata in the triangular border region of Sichuan,Gansu and Shaanxi provinces,as so -called golder trangle,coith many gold deposits or occurrences similar to the Zhaishang deposit,it is obviously of great importance to evaluate the value of tungsten and other elements in these gold deposits.
【Fund】: 国家重点基础研究发展规划项目(2006CB403500);; 国家自然科学基金项目(40773036);; 高等学校学科创新引智计划项目(B07011);; 教育部长江学者和创新团队、中国人民武装警察部队黄金指挥部勘查项目资助
【CateGory Index】: P618.51
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