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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
【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
【Key words】 quartz and calcite veins; minor element geochemistry; Longmenshan orogen;
- 【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