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《Mineral Deposits》 2014-01
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Typomorphic characteristics of gold-bearing minerals in Zhesang gold deposit, Yunnan Province

DAI HongZhang;CHEN CuiHua;GU XueXiang;LI BaoHua;DONG ShuYi;CHENG WenBin;State Key Laboratory of Geological Processes and Resources, School of Earth Sciences and Resources, China University of Geosciences;College of Earth Sciences, Chengdu University of Technology;  
The Zhesang gold deposit located in the structural belt of Yunnan-Guizhou-Guangxi gold triangle structural belt.The formation of the Zhesang gold deposit experienced three stages,i.e.,sedimentary diagenesis,hydrothermal mineralization and supergenic oxidation.Pyrites and arsenopyrites are two major Au-bearing minerals.Petrographic and typomorphic observations reveal that arsennopyrites were formed in the hydrothermal mineralizationⅠphase(HMⅠ)whereas pyrites in the hydrothermal mineralizationⅡphase(HMⅡ),which was the primary gold formation phase.The gold-bearing pyrites are colloidal,fine-gained or fragmentized,while the gold-bearing arsenopyrites are in the coarse columnar form.Both of them have low reflectance.Lattice parameter measurement indicates that theaof pyrite is 5.4300~5.4325,which gradually becomes larger from HMⅠto HMⅡ,suggesting that As was concentrated in the hydrothermal mineralization stage.Gold-bearing arsenopyrites are rich in S,Co and poor in As and,as a result,b,candβare lower than their theoretical values.Similarities of geochemical and S isotopic compositions between pyrites and arsenopyrites imply that organic wall rock contributed most of the metallogenic materials.It is thus concluded that the Zhesang gold deposit is a middle-low temperature hydrothermal deposit.
【Fund】: 国家自然科学基金重点项目(编号:40930423);国家自然科学基金面上项目(编号:41372093);; 国家重点基础研究发展计划(973)(编号:2014CB440903);; 教育部高校博士点基金项目(编号:2009512212000);; 成都理工大学中青年骨干教师培养计划项目;; 高等教育质量工程项目《矿相学》优秀教材建设(编号:XJC1105)联合资助
【CateGory Index】: P618.51
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