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Genesis and mineralization of gold-bearing quartz veins in the Xiao Qinling area,central China

查看全文 作  者:LIANG [1,2]Jiwei;LI [1,2]Rongxi;ZHANG [1,2]Shaoni;CHEN [1,2]Baoyun;DUAN [1,2]Lizhi;Pierre [3]Thibault 高影响力作者 机构地区:[1]School of Earth Science andResource,Chang'an University,Xi'an 710054,China;[2]Key Laboratory of West Mineral Resorce&Geology Engineering,Education Ministry of China,Chang'an University,Xi'an 710054,China;[3]Kecui Mining Development Company,Shanghai 200000,China高影响力机构 出  处:《Chinese Journal Of Geochemistry》索引2012年第31卷第4期,共8页高影响力期刊 基  金:supported jointly by the CNSF (No. 41173055);the National Basic Research Program of China (No.2003CB214605) 摘  要:Gold-bearing quartz veins of the Taihua Group consisting of Archean metavolcanic rocks are a main gold deposit type in the Xiao Qinling area,one of the three biggest gold production areas in China.The quartz veins experienced strong alteration characterized by a typical mesothermal hydrothermal altered mineral assemblage.The grade of gold is affected by the contents of sulphides,e.g.galena,pyrite and chalcopyrite.Results of minor elements analysis for the of gold-bearing quartz veins indicate higher contents of Au and high contents of Ag,Pb,Cu,Cd,W,and Mo.Abundant fluid inclusions were found in the gold-bearing quartz veins.Three types of fluid inclusions were identified:(1) aqueous inclusions;(2) CO 2-bearing inclusions;and(3) daughter crystal-bearing fluid inclusions.Homogenization temperatures ranged from 110 to 670℃ with low and high peaks appearing at 160 180℃ and 280 300℃,respectively.The salinity of aqueous inclusions varies between 1.8 wt% and 38.2 wt% NaCl.The homogenization temperature and salinity show a positive correlation.The H and O isotopes of fluid inclusions in the gold-bearing quartz veins indicate that magmatic solution and metamorphic hydrothermal solution,together with meteoric water,were involved in the formation of gold-bearing fluid.Mesozoic magma activities related to granite intrusions should be the main source of CO 2 fluid with higher temperature and salinity. 关 键 词:含金石英脉 小秦岭地区 成矿作用 中国 流体包裹体 重量百分比 成因 盐度变化
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