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    贵州织金含稀土磷矿床的Sm-Nd同位素年龄及其地质意义

    施春华 胡瑞忠

    施春华, 胡瑞忠, 2008. 贵州织金含稀土磷矿床的Sm-Nd同位素年龄及其地质意义. 地球科学, 33(2): 205-209.
    引用本文: 施春华, 胡瑞忠, 2008. 贵州织金含稀土磷矿床的Sm-Nd同位素年龄及其地质意义. 地球科学, 33(2): 205-209.
    SHI Chun-hua, HU Rui-zhong, 2008. Samarium-Neodymium Radiometric Dating and Its Geologic Implication of the Zhijin REE-Bearing Phosphorites, Guizhou Province, Southwest China. Earth Science, 33(2): 205-209.
    Citation: SHI Chun-hua, HU Rui-zhong, 2008. Samarium-Neodymium Radiometric Dating and Its Geologic Implication of the Zhijin REE-Bearing Phosphorites, Guizhou Province, Southwest China. Earth Science, 33(2): 205-209.

    贵州织金含稀土磷矿床的Sm-Nd同位素年龄及其地质意义

    基金项目: 

    中国科学院知识创新工程重要方向项目 KZCX3-SW-125

    浙江林学院科学研究发展基金项目 2351000584

    详细信息
      作者简介:

      施春华(1976-), 女, 目前主要从事旅游环境地球化学等教学与科研工作.E-mail: shichunhua7924@163.com

    • 中图分类号: P597

    Samarium-Neodymium Radiometric Dating and Its Geologic Implication of the Zhijin REE-Bearing Phosphorites, Guizhou Province, Southwest China

    • 摘要: 为探讨贵州织金含稀土磷矿床的形成时间和成矿物源, 利用Sm-Nd同位素稀释法对该矿床磷块岩中6个小壳化石及胶磷矿样品进行了年龄测定.样品的质谱分析测试结果显示, 样品的147Sm/144Nd与143Nd/144Nd构成了一条相关性良好的线性等时线; 计算结果表明织金含稀土磷矿床具有533±22Ma的Sm-Nd等时年龄, εNd (t) 值为-2.44~-2.77, 表明它们具有相同的成因和相近的形成时代, 本次测得年龄代表着真实的成矿年龄; 二阶段Nd的模式年龄为1313~1338Ma.结合前人对该矿床稀土元素地球化学的研究成果表明, 织金含稀土磷矿床的成矿物源有新生地幔物质组分的加入.

       

    • 图  1  织金含稀土磷矿床地质简图及采样位置

      1.三叠系; 2.二叠系; 3.石炭系; 4.寒武系明心寺组; 5.寒武系牛蹄塘组; 6.震旦系灯影组; 7.地层界线; 8.断层; 9.采样位置

      Fig.  1.  Geological sketch map of the Zhijin

      图  2  样品的Sm-Nd等时线

      Fig.  2.  Sm-Nd isochron for the sample

      表  1  样品的Sm、Nd同位素测定结果

      Table  1.   Sm, Nd isotopic compositions of samples

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    • 收稿日期:  2007-05-25
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