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大兴安岭中生代花岗岩类的地球化学

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林强 葛文春 吴福元 孙德有 曹林. 大兴安岭中生代花岗岩类的地球化学[J]. 岩石学报, 2004, 20(3): 403-412.
引用本文: 林强 葛文春 吴福元 孙德有 曹林. 大兴安岭中生代花岗岩类的地球化学[J]. 岩石学报, 2004, 20(3): 403-412.
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IIN Qiang,GE WenChun,WU FuYuan,SUN DeYou,CA0 Lin College of Earth Sciences,Jilin University,Changchun 130061,China. Geochemistry of Mesozoic granites in Da Hinggan Ling ranges[J]. Acta Petrologica Sinica, 2004, 20(3): 403-412.
Citation: IIN Qiang,GE WenChun,WU FuYuan,SUN DeYou,CA0 Lin College of Earth Sciences,Jilin University,Changchun 130061,China. Geochemistry of Mesozoic granites in Da Hinggan Ling ranges[J]. Acta Petrologica Sinica, 2004, 20(3): 403-412.
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大兴安岭中生代花岗岩类的地球化学

    • 吉林大学地球科学学院 长春130061(林强，葛文春，吴福元，孙德有)，吉林大学地球科学学院 长春130061(曹林)

  • 基金项目:

    国家自然科学基金(49972027)

Geochemistry of Mesozoic granites in Da Hinggan Ling ranges

    摘要
  • 大兴安岭中生代花岗岩根据微量元素地球化学特征划分为高锶花岗岩类和低锶花岗岩类，前者富集Ba、Sr、Ti，而后者强烈亏损这些元素而富集大离子亲石元素和高场强元素。高锶花岗岩类主要由石英闪长岩、英云闪长岩和花岗闪长岩组成，属于Ⅰ型花岗岩；低锶花岗岩类由二长花岗岩、正长花岗岩、碱长花岗岩和碱性花岗岩组成，二长花岗岩一正长花岗岩一碱长花岗岩也属于Ⅰ型花岗岩，碱性花岗岩为A1型花岗岩。这两类花岗岩均显示εNd(t)正值^87Sr／^86Sr低值以及较低的Nd模式年龄。高锶与低锶花岗岩类地球化学差异性表明，高锶花岗岩起源于相对亏损的幔源岩浆的分异作用，而低锶花岗岩类的源区与显生宙地壳增生时期起源于地幔的年轻地壳物质有关，即起源于富集型幔源基性岩石的部分熔融。大兴安岭中生代花岗岩与流纹岩之间地球化学相似性以及与玄武岩类的相关性表明，它们是统一的构造一岩浆体系的产物，共同制约于古亚洲洋闭合后的大陆伸展的构造环境和闭合期间壳幔相互作用形成的地幔源区。
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修回日期:  2002-10-25
刊出日期:  2004-05-31

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