大兴安岭东北部侏罗纪花岗质岩石的锆石U-Pb年龄、地球化学特征及成因

隋振民 葛文春 吴福元 张吉衡 徐学纯 程瑞玉. 大兴安岭东北部侏罗纪花岗质岩石的锆石U-Pb年龄、地球化学特征及成因[J]. 岩石学报, 2007, 23(2): 461-480.
引用本文: 隋振民 葛文春 吴福元 张吉衡 徐学纯 程瑞玉. 大兴安岭东北部侏罗纪花岗质岩石的锆石U-Pb年龄、地球化学特征及成因[J]. 岩石学报, 2007, 23(2): 461-480.
Zircon U-Pb ages, geochemistry and its petrogenesis of Jurassic granites in northeastern part of the Da Hinggan Mts.[J]. Acta Petrologica Sinica, 2007, 23(2): 461-480.
Citation: Zircon U-Pb ages, geochemistry and its petrogenesis of Jurassic granites in northeastern part of the Da Hinggan Mts.[J]. Acta Petrologica Sinica, 2007, 23(2): 461-480.

大兴安岭东北部侏罗纪花岗质岩石的锆石U-Pb年龄、地球化学特征及成因

  • 基金项目:

    本文为国家自然科学基金(40372038,40325006)和国家油气专项(XQ2004-07)项目研究成果.致谢感谢中国科学院地质与地球物理研究所毛骞在锆石CL图像采集、西北大学地质学系柳小明在锆石U-Pb测试及中国科学院广州地球化学研究所刘颖和涂湘林在主、微量元素分析过程中的帮助.

Zircon U-Pb ages, geochemistry and its petrogenesis of Jurassic granites in northeastern part of the Da Hinggan Mts.

  • 大兴安岭东北部花岗岩锆石的LA-ICPMS U-Pb年龄测定结果表明,前人划分的元古代、早古生代和晚古生代的花岗岩有相当一部分是侏罗纪花岗岩.根据时间先后关系,可将本区侏罗纪花岗岩的侵位顺序划分为早、晚两期,其锆石U-Pb年龄分别为188~190 Ma和171~181 Ma,这些侏罗纪花岗岩的年龄数据与东北其它地区侏罗纪花岗岩完全可以对比.在地球化学特征上可以将这些花岗质岩石划分为低Sr高Yb型和高Sr低Yb型两类,它们有相同或相似的源岩组成而起源的深度不同,早期侵入的花岗岩为低Sr高Yb型,起源于压力较低的中地壳,而晚期侵入的花岗岩为高Sr低Yb型,类似于"C"型埃达克岩,起源于压力较高的下地壳.锆石Hf同位素成分特征表明,侏罗纪花岗岩的源区物质主要为新元古代和显生宙期间增生的地壳物质及两期增生地壳物质的混合物.本区侏罗纪花岗岩以花岗闪长岩-二长花岗岩为主,为准铝质或弱过铝质、高钾钙碱性系列的Ⅰ型花岗岩,具有类似于活动大陆边缘花岗岩的岩石组合特征,属于呈北北东向带状展布的中国东北地区侏罗纪花岗岩带的一部分,其形成与古太平洋板块的俯冲作用有关.
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修回日期:  2006-09-12
刊出日期:  2007-02-28

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