冀北闪长质岩石的锆石SHRIMP U-Pb年龄:晚古生代岩浆弧的地质记录

王惠初 赵凤清 李惠民 孙立新 苗来成 冀世平. 冀北闪长质岩石的锆石SHRIMP U-Pb年龄:晚古生代岩浆弧的地质记录[J]. 岩石学报, 2007, 23(3): 597-604.
引用本文: 王惠初 赵凤清 李惠民 孙立新 苗来成 冀世平. 冀北闪长质岩石的锆石SHRIMP U-Pb年龄:晚古生代岩浆弧的地质记录[J]. 岩石学报, 2007, 23(3): 597-604.
Zircon SHRIMP U-Pb age of the dioritic rocks from northern Hebei: the geological records of late Paleozoic magmatic arc[J]. Acta Petrologica Sinica, 2007, 23(3): 597-604.
Citation: Zircon SHRIMP U-Pb age of the dioritic rocks from northern Hebei: the geological records of late Paleozoic magmatic arc[J]. Acta Petrologica Sinica, 2007, 23(3): 597-604.

冀北闪长质岩石的锆石SHRIMP U-Pb年龄:晚古生代岩浆弧的地质记录

  • 基金项目:

    中国地质调查局华北重要经济区基础地质综合研究项目(1212010510512)和国家自然科学基金项目(40373032)资助.致谢成文过程中得到了赵越研究员和张栓宏博士的热情帮助,评审员对文稿提出了宝贵的修改意见,在此深表谢忱.

Zircon SHRIMP U-Pb age of the dioritic rocks from northern Hebei: the geological records of late Paleozoic magmatic arc

  • 华北克拉通北缘的丰宁-承德地区分布着许多被认为是古元古代的片麻状闪长质-石英闪长质-花岗闪长质侵入体,新的年代学资料揭示这些侵入体中许多是晚古生代的产物.本次工作从京北喇叭沟门闪长岩体和丰宁天桥含石英闪长岩体中分别获得了(288.0±4.8)Ma和(279.5±5.6)Ma的锆石SHRIMP U-Pb年龄.这些钙碱性岩石的存在表明华北克拉通北缘在早二叠世是一条安第斯型的活动大陆边缘.综合分析冀北地区晚古生代侵入岩的侵位时代和变形特点,结合该地区晚古生代发生变形变质作用的年龄信息,推测华北克拉通北侧的古亚洲洋在晚二叠世末封闭,随后进入了主造山期之后的构造松弛阶段.
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修回日期:  2006-08-17
刊出日期:  2007-03-31

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