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    太古宙—元古宙过渡分界及成矿动力体制转换

    邓军 孙忠实 王建平 王庆飞 王喜臣 燕长海

    邓军, 孙忠实, 王建平, 王庆飞, 王喜臣, 燕长海, 2003. 太古宙—元古宙过渡分界及成矿动力体制转换. 地球科学, 28(1): 87-96.
    引用本文: 邓军, 孙忠实, 王建平, 王庆飞, 王喜臣, 燕长海, 2003. 太古宙—元古宙过渡分界及成矿动力体制转换. 地球科学, 28(1): 87-96.
    DENG Jun, SUN Zhong-shi, WANG Jian-ping, WANG Qing-fei, WANG Xi-chen, YAN Zhang-hai, 2003. Demarcating Interval between Archean Group and Proterozoic Group and Ore-Forming Dynamical Transformation. Earth Science, 28(1): 87-96.
    Citation: DENG Jun, SUN Zhong-shi, WANG Jian-ping, WANG Qing-fei, WANG Xi-chen, YAN Zhang-hai, 2003. Demarcating Interval between Archean Group and Proterozoic Group and Ore-Forming Dynamical Transformation. Earth Science, 28(1): 87-96.

    太古宙—元古宙过渡分界及成矿动力体制转换

    基金项目: 

    国家自然科学基金 40172036

    国家重点基础研究发展规划项目 1999043206

    教育部“科学技术研究重点项目 01037

    详细信息
      作者简介:

      邓军(1958—),男,教授,博士生导师,构造地质学和矿床学专业,主要从事区域构造、成矿流体及成矿动力学的教学和科研工作

    • 中图分类号: P541;P61

    Demarcating Interval between Archean Group and Proterozoic Group and Ore-Forming Dynamical Transformation

    • 摘要: 太古宙与元古宙之间分界时限较窄、测年数据偏新和混乱, 极大遏制了地球早期基础地质的深入研究.通过太古宙与元古宙分界标志和过渡标志的确定, 将太古代—元古代间动力体制转换类型划分为4种: 挤压体制向扩张体制转换; 垂直运动与水平运动间转换; 水平主压应力场转换; 地幔柱体制向板块构造体制转换.太古代与元古代间动力体制转换产物主要为真核生物、放射性元素、岩浆、矿产, 各自形成时限可达(3~5) × 108 a.太古宙与元古宙之间分界不应以单一年代划分, 而是一个渐变过渡的界线, 可初步确定在2.2 0~2.80Ga之间.太古宙—元古宙界线的划分应与地球动力学和构造体制等重大事件相联系, 此研究为探求早期深部成矿作用带来新的启迪

       

    • 图  1  吉林板石沟地区地质图

      1.古元古代盖层; 2.变黑云钾长花岗岩及角闪-绿片岩相韧变带; 3.中粒英云闪长岩角闪岩相线韧变带; 4.断裂及产状; 5.绿片岩相韧变带; 6.地质界线

      Fig.  1.  Geology sketch of Banshigou area, Jilin Province

      图  2  变质上壳岩系Sm-Nd等时线

      Fig.  2.  Sm-Nd isochronism graph of metamorphic supracrust systems

      表  1  变质上壳岩系Sm-Nd年龄测试与计算结果

      Table  1.   Sm-Nd age-dating and calculating values in metamorphic supracrustal systems

      表  2  黑云长英片麻岩锆石年龄测定与计算结果

      Table  2.   Acorite age-dating and calculating values of biotite felsite gneiss

      表  3  变黑云母钾长花岗岩锆石年龄测定与计算结果

      Table  3.   Acorite age-dating and calculating values of metamorphic biotite potash feldspar granite

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    • 收稿日期:  2002-03-11
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