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《Earth and Environment》 2009-01
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The Characteristics of Fluid Inclusions from the Yinan Gold Deposit,Shandong Province and Their Geological Significance

LIU Li1,GU Xue-xiang1,LI Bao-hua2,DONG Shu-yi1,2(1.College of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China;2.College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China)  
Based on fluid inclusion study,this paper made further discussions on the source of ore-forming materials and the ore genesis of the Yinan gold deposit,Shandong Province.Petrographic observations and microthermometric data indicated that the main types of fluid inclusions are aqueous inclusions,CO2-H2O inclusions,crystalline melt inclusions and daughter mineral-bearing multiphase inclusions trapped in four mineralization stages.Melt inclusions were recognized in garnet,epidote and quartz.In the first and second mineralization stages,the ore-forming fluid was characterized by high temperature and high salinity,with the homogenization temperatures of 430~510℃ and 330~390 ℃,respectively and the salinities of 56.7 wt% NaCl and 2.2~53.5 wt% NaCl,respectively.In the third mineralization stage,the ore-forming fluid was characterized by moderate to low temperatures(190~250℃) and large variations in salinity(6.45~53.5 wt% NaCl).In the last mineralization stage,the homogenization temperatures ranged from 130℃ to 190℃,with salinities ranging from 2.07 to 15.76 wt% NaCl.The assemblage of different fluid inclusions and the evolution characteristics of fluid inclusions showed that fluid immiscibility was the main cause for mineralization and that the ore-forming fluids were dominated by magmatic hydrothermal water.
【Fund】: 国家自然科学基金(40772060);; 中国地质调查局危机矿山接替资源找矿项目(200637035);; 高等学校学科创新引智计划(B07011);; 中国地质大学地质过程与矿产资源国家重点实验室基金(GPMR0531)
【CateGory Index】: P618.51
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