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龙门山造山带中段石英方解石脉的微量元素地球化学特征

MINOR ELEMENT GEOCHEMISTRY FOR QUARTZ AND CALCITE VEINS FROM THE MIDDLE LONGMENSHAN OROGEN

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【作者】 黄永健张成江汪云亮刘树根赵锡奎王国芝

【Author】 Huang Yongjian Zhang Chengjiang Wang Yunliang (Department 3 , Chengdu Institute of Technology) Liu Shugen Zhao Xikui ( Department of Petroleum Geology , Chengdu Institute of Technology) Wang Guozhi (Department of Geology ,

【机构】 成都理工学院

【摘要】 本文讨论了龙门山造山带中段上孟—漩口一线石英方解石脉的微量元素地球化学特征。结果表明:与方解石相比,石英杂质元素总量很低,特别是稀土元素含量远低于方解石,但K、Na、Cr、Co、Th 等则变化不大;石英与方解石均富集重稀土;石英与方解石的稀土元素配分型式总体相似,暗示其来源之间有一定的联系;石英和方解石脉均有强的铕正异常,不同层位的样品铕正异常强度不同,指示围岩条件的差异及形成条件的影响。

【Abstract】 This paper discusses minor element geochemistry for quartz and calcite veins from Shangmeng Xuankou sector of the middle Longmenshan orogen The results indicate that:1 in comparison with calcite veins,only a very low content of minor elements,especially REE,is kept in quartz veins,while contents of K,Na,Cr,Co Th,U,As,Sb are almost same in both veins;2 relative enrichment in HREE is shown in both veins;3 REE partitioning patterns of both veins are very similar to each other which indicates some relations of their sources;4 Both quattz and calcife veins show very strong positiveu Eu anomaly with anomaly intensity varying with sampling layers which reflects the effect of host rocks and veining conditions

  • 【文献出处】 四川地质学报 ,ACTA GEOLOGICA SICHUAN , 编辑部邮箱 ,1999年04期
  • 【分类号】P595
  • 【被引频次】10
  • 【下载频次】371
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