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冀北隆化早前寒武纪高级变质区内的晚古生代片麻状花岗闪长岩--锆石SHRIMP U-Pb年龄及其构造意义

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文章导航 > 岩石学报 > 2004 > 20(3): 621-626

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张拴宏　赵越　宋彪　吴海. 冀北隆化早前寒武纪高级变质区内的晚古生代片麻状花岗闪长岩--锆石SHRIMP U-Pb年龄及其构造意义[J]. 岩石学报, 2004, 20(3): 621-626.
引用本文: 张拴宏　赵越　宋彪　吴海. 冀北隆化早前寒武纪高级变质区内的晚古生代片麻状花岗闪长岩--锆石SHRIMP U-Pb年龄及其构造意义[J]. 岩石学报, 2004, 20(3): 621-626.
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ZHANG ShuanHong,ZHA0 Yue,S0NG Biao,WU Hai Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,China Beijing SHRIMP Center and Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China Geological Information Center,Ministry of Land and Resource,Yanjiao 065201,China. The late Paleozoic gneissic granodiorite pluton in early Pre-cambrian high-grade metamorphic terrains near Longhua county in northern Hebei province, north China: result from zircon SHRIMP U-Pb dating and its tectonic implications[J]. Acta Petrologica Sinica, 2004, 20(3): 621-626.
Citation: ZHANG ShuanHong,ZHA0 Yue,S0NG Biao,WU Hai Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081,China Beijing SHRIMP Center and Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China Geological Information Center,Ministry of Land and Resource,Yanjiao 065201,China. The late Paleozoic gneissic granodiorite pluton in early Pre-cambrian high-grade metamorphic terrains near Longhua county in northern Hebei province, north China: result from zircon SHRIMP U-Pb dating and its tectonic implications[J]. Acta Petrologica Sinica, 2004, 20(3): 621-626.
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冀北隆化早前寒武纪高级变质区内的晚古生代片麻状花岗闪长岩--锆石SHRIMP U-Pb年龄及其构造意义

    • 中国地质科学院地质力学研究所，中国地质科学院地质力学研究所，北京离子探针中心中国地质科学院地质研究所，国土资源部实物地质资料中心 北京 100081，北京 100081，北京100037，河北燕郊065201

  • 基金项目:

    国家自然科学基金(40132020)，国土资源地质大调查项目(DKD2001008)资助

The late Paleozoic gneissic granodiorite pluton in early Pre-cambrian high-grade metamorphic terrains near Longhua county in northern Hebei province, north China: result from zircon SHRIMP U-Pb dating and its tectonic implications

    摘要
  • 本文报道了冀北隆化早前寒武纪高级变质区中片麻状花岗闪长岩的SHRIMP U-Ph锆石年龄为311±2Ma(95％置信度)。锆石为典型的岩浆结晶锆石,少量继承锆石年龄平均为 1809±21 Ma(95％置信度),与华北克拉通的形成年龄接近,可能与本区早元古代末华北克拉通的最后拼合有关。冀北隆化早前寒武纪高级变质区中晚古生代片麻状花岗闪长岩的确定说明:内蒙古隆起(即“内蒙地轴”)实际为晚古生代-早中生代期间构造变形及剥露的结果。这一发现对于认识燕山构造带的早期演化历史有重要意义。
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修回日期:  2003-10-17
刊出日期:  2004-05-31

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