栖霞市马家窑金矿床成矿流体地球化学特征
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Geochemical Characteristics of Ore-forming Fluid in Majiayao Gold Deposit in Qixia City
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    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H2O,CO2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。

    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 H2O and CO2, 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.

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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].山东国土资源,2008,24(1):

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