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《Acta Scientiarum Naturalium Universitatis Pekinensis》 2010-04
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Study on Characteristics of Ore-Forming Fluid and Chronology in the Yindu Ag-Pb-Zn Polymetallic Ore Deposit,Inner Mongolia

CHANG Yong,LAI Yong The Key Laboratory of Orogenic Belts and Crustal Evolution,Ministry of Education,School of Earth and Space Sciences,Peking University,Beijing 100871  
Yindu Ag-Pb-Zn polymetallic ore deposit,Inner Mongolia,is a oversize silver deposit.The ore-forming process includes three stages,i.e.the early,middle and late stages,which are characterized by mineral assemblages of sphalerite-pyrrhotite-chalcopyrite,galena-pyrrhotite and fluorite-muscovite-carbonate,respectively.The early stage is the main mineralizing stage related to Cu and Zn mineralization,the middle stage is related to Ag,Pb and Zn mineralization,and the last stage,the end of ore-forming process,has weak mineralization.Through the analysis of Laser Raman microprobe,it shows that the ore-forming fluid is H2 O-CO2 -CH4 -NaCl system.Based on fluid inclusion study,it has been recognized that the ore-forming hydrothermal fluid has the features like low salinity(2% -5%),low density(0.72-0.88g/cm3).With the evolution of ore-forming hydrothermal fluid,ore-forming temperature decreases gradually.The temperature of early,middle and last stage is 340.5℃,282.4℃ and 260.3℃,respectively.The ore-forming pressures are from 37 to 74 km,which reflect the mineralizing depth ranges from 3.7 to 7.0 km.The muscovite 40 Ar/39 Ar age is 135±3 Ma(early Cretaceous),which is analyzed by laser 40 Ar/39 Ar method.
【Fund】: 国家重点基础研究发展计划项目(2006CB403501);; 中国地质调查局项目(1212010813045)资助
【CateGory Index】: P618.2
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