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石英、黄铁矿及其包裹体的稀土元素特征——以胶东焦家式金矿为例

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文章导航 > 岩石学报 > 2003 > 19(2): 267-274

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李厚民 沈远超 毛景文 刘铁兵 朱和平. 石英、黄铁矿及其包裹体的稀土元素特征——以胶东焦家式金矿为例[J]. 岩石学报, 2003, 19(2): 267-274.
引用本文: 李厚民 沈远超 毛景文 刘铁兵 朱和平. 石英、黄铁矿及其包裹体的稀土元素特征——以胶东焦家式金矿为例[J]. 岩石学报, 2003, 19(2): 267-274.
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REE features of quartz and pyrite and their fluid inclusions: an example of Jiaojia-type gold deposits, northwestern Jiaodong peninsula.[J]. Acta Petrologica Sinica, 2003, 19(2): 267-274.
Citation: REE features of quartz and pyrite and their fluid inclusions: an example of Jiaojia-type gold deposits, northwestern Jiaodong peninsula.[J]. Acta Petrologica Sinica, 2003, 19(2): 267-274.
shu

石英、黄铁矿及其包裹体的稀土元素特征——以胶东焦家式金矿为例

    • [1]中国地质大学（北京）地球科学与资源学院，北京100083 [2]长安大学，西安710054 [3]中国科学院地质与地球物理研究所，北京100029 [4]中国科学院矿物资源探查研究中心，北京100101

  • 基金项目:

    中国科学院黄金“九五”重大项目“山东重要金成矿区的成矿模式及找矿预测”(KZ951-A1-404-02-02)，中国科学院创新工程项目“金矿资源战略接替基地若干靶区预测”(KZCX1-Y-03-01)资助

REE features of quartz and pyrite and their fluid inclusions: an example of Jiaojia-type gold deposits, northwestern Jiaodong peninsula.

    摘要
  • 本文采用ICP—MS测定了焦家、马塘、东季、红布等焦家式金矿床中黄铁矿、石英及其包裹体的稀土元素组成。结果表明：采用ICP—MS直接测定黄铁矿包裹体的稀土元素是可行的；包裹体爆裂丰度虽然对稀土总量有影响，但矿源稀土元素背景值的差异也是流体中稀土总量差别的主要原因之一。∑REE、δEu、δCe及LREE／HREE、(La/Yb)N、(Ce/Yb)N、(La／Lu)N都是有意义的稀土元素特征参数；焦家式金矿同一成矿阶段黄铁矿、石英及其包裹体的稀土元素特征相似，显示了它们的同源特征；不同成矿阶段黄铁矿、石英及其包裹体的稀土元素特征有差异，反映了其成矿流体特征的差异。
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    • 参考文献(24)
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修回日期:  2002-11-20
刊出日期:  2003-05-31

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