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栖霞市马家窑金矿床成矿流体地球化学特征
引用本文:胡伟华,邱介玲,程鑫,林永芸.栖霞市马家窑金矿床成矿流体地球化学特征[J].山东地质,2008(1):26-29.
作者姓名:胡伟华  邱介玲  程鑫  林永芸
作者单位:山东省第三地质矿产勘查院,山东烟台264003
摘    要:马家窑金矿床是胶东地区比较典型的石英脉型金矿床代表,属中低温热液矿床,成矿流体盐度较低,气相成分以H2O,CO2为主,其次是Na^+,Ca^+和Cl^-,K^+和F^-较贫,流体的成分与大气降水热液相类似。成矿流体的H,O同位素值则反映大气降水在不同温度和不同水/岩值条件下与栖霞超单元回龙夼单元交换后的分布特征,认为马家窑金矿床的成矿热液属大气降水成因。

关 键 词:马家窑金矿床  石英脉型金矿  大气降水  流体  包裹体  山东栖霞

Geochemical Characteristics of Ore - forming Fluid in Majiayao Gold Deposit in Qixia City
Institution:HU Wei - hua, QIU Jie - ling, CHENG Xin, LIN Yong - yun ( No. 3 Exploration Institute of Geology and Mineral Resources, Shandong Yantai 264003, China)
Abstract:Majiayao gold deposit is the representative of typical quartz vein type gold deposits, which blongs to low temperature thermal deposit. Salinity of ore - forming fluid is rather low, and vapor phase compositions are majorly composed of H2O and COE, accompanying with Na^+ , Ca^+ , K^+ and F^-. Components of fluid is similar with meteoric water. Isotopic values of H and O in ore - forming fluid reflect distribution characteristics of meteoric water under different temperature, water and rock values after being changed with Huilongkuang unit of Qixia superunit. It is regarded that ore - forming hydrothermal solution of Majiayao gold deposit is meteoric water hydrothermal solution.
Keywords:Majiayao gold deposit  quartz vein gold deposit  meteoric water  fluid  inclusion  Qixia in Shandong province
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