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吉林黄泥岭花岗岩体的单颗粒锆石U—Pb年龄

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文章导航 > 岩石学报 > 2002 > 18(4): 475-481

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张艳斌,吴福元,李惠民,路孝平,孙德有,周红英. 吉林黄泥岭花岗岩体的单颗粒锆石U—Pb年龄[J]. 岩石学报, 2002, 18(4): 475-481.
引用本文: 张艳斌,吴福元,李惠民,路孝平,孙德有,周红英. 吉林黄泥岭花岗岩体的单颗粒锆石U—Pb年龄[J]. 岩石学报, 2002, 18(4): 475-481.
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ZHANG YanBin 1,WU FuYuan 1,LI HuiMin 2,LU XiaoPing 3,SUN DeYou 1 and ZHOU HongYing 21. College of Earth Sciences,Jilin University,Changchun 130061,China, 2. Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin 300170,China, 3. Institute of Regional Geology and Mineral Resources Survey of Jilin Province,Changchun 130022,China.. Single grain zircon U-Pb ages of the Huangniling granite in Jilin province[J]. Acta Petrologica Sinica, 2002, 18(4): 475-481.
Citation: ZHANG YanBin 1,WU FuYuan 1,LI HuiMin 2,LU XiaoPing 3,SUN DeYou 1 and ZHOU HongYing 21. College of Earth Sciences,Jilin University,Changchun 130061,China, 2. Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin 300170,China, 3. Institute of Regional Geology and Mineral Resources Survey of Jilin Province,Changchun 130022,China.. Single grain zircon U-Pb ages of the Huangniling granite in Jilin province[J]. Acta Petrologica Sinica, 2002, 18(4): 475-481.
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吉林黄泥岭花岗岩体的单颗粒锆石U—Pb年龄

    • 吉林大学地球科学学院 长春130061(张艳斌，吴福元，孙德有)，中国地质调查局天津地质矿产研究所 天津300170(李惠民)，吉林省地质勘察局区域地质矿产调查研究所 长春130022(路孝平)，中国地质调查局天津地质矿产研究所 天津300170(周红英)

  • 基金项目:

    中国地质调查局综合研究项目 ( 2 0 0 1 1 30 0 0 0 52 )，国家自然科学基金项目 ( 49872 0 31 )研究成果

Single grain zircon U-Pb ages of the Huangniling granite in Jilin province

    摘要
  • 在华北地台北缘与其北侧兴蒙造山带的结合部位 ,发育有大量的所谓“加里东期”花岗岩 ,其中以出露在吉林省中部的黄泥岭岩体最为典型。然而 ,高精度的单颗粒锆石 U-Pb定年结果显示 ,采自黄泥岭岩体不同部位的三个样品的同位素年龄分别为 168± 3 Ma、153± 2 Ma和 158± 3 Ma,说明黄泥岭岩体并不是形成于早古生代 ,而是形成于中生代的中 -晚侏罗世。结合前人获得的 166± 2 Ma的锆石 SHRIMP U-Pb年龄 ,本文认为 ,黄泥岭岩体是在 150～ 170 Ma之间由至少两期岩浆活动形成的复式岩体。这一中生代年代学结果的获得 ,表明华北地台与北侧佳木斯地块或东侧兴凯地块间拼合历史的传统模式需要进一步
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修回日期:  2001-09-24
刊出日期:  2002-11-30

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