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北祁连造山带西段车路沟岩体U-Pb年代学、地球化学特征及岩石成因

樊新祥, 孔维琼, 杨镇熙, 赵吉昌, 李昱星. 2020. 北祁连造山带西段车路沟岩体U-Pb年代学、地球化学特征及岩石成因[J]. 中国地质, 47(3): 755-766. doi: 10.12029/gc20200314
引用本文: 樊新祥, 孔维琼, 杨镇熙, 赵吉昌, 李昱星. 2020. 北祁连造山带西段车路沟岩体U-Pb年代学、地球化学特征及岩石成因[J]. 中国地质, 47(3): 755-766. doi: 10.12029/gc20200314
FAN Xinxiang, KONG Weiqiong, YANG Zhenxi, ZHAO Jichang, LI Yuxing. 2020. U-Pb chronology, geochemical characteristics and petrogenesis of the Chelugou pluton in the western part of North Qilian orogenic belt[J]. Geology in China, 47(3): 755-766. doi: 10.12029/gc20200314
Citation: FAN Xinxiang, KONG Weiqiong, YANG Zhenxi, ZHAO Jichang, LI Yuxing. 2020. U-Pb chronology, geochemical characteristics and petrogenesis of the Chelugou pluton in the western part of North Qilian orogenic belt[J]. Geology in China, 47(3): 755-766. doi: 10.12029/gc20200314

北祁连造山带西段车路沟岩体U-Pb年代学、地球化学特征及岩石成因

  • 基金项目:
    中国地质调查局项目“祁连成矿带肃南—大柴旦地区地质矿产调查”(DD20160012)资助
详细信息
    作者简介: 樊新祥, 男, 1972年生, 高级工程师, 从事矿产地质调查及矿产勘查工作; E-mail:1411372056@qq.com
    通讯作者: 孔维琼, 男, 1987年生, 硕士, 工程师, 从事矿产地质调查及矿产勘查工作; E-mail:277890759@qq.com
  • 中图分类号: P597;P588.1

U-Pb chronology, geochemical characteristics and petrogenesis of the Chelugou pluton in the western part of North Qilian orogenic belt

  • Fund Project: Supported by China Geological Survey Project(No.DD20160012)
More Information
    Author Bio: FAN Xinxiang, male, born in 1972, senior engineer, engages in geological survey and mineral exploration; E-mail:1411372056@qq.com .
    Corresponding author: KONG Weiqiong, male, born in 1987, master, engages in geological survey and mineral exploration; E-mail:277890759@qq.com
  • 车路沟岩体位于北祁连造山带最西端,岩石类型以英云闪长玢岩和闪长玢岩为主。本次对英云闪长玢岩进行U-Pb年代学研究,获得加权平均年龄为(462.1±3.8)Ma,表明岩体形成于中奥陶世。岩石地球化学分析结果显示,英云闪长玢岩中SiO2含量60.37%~66.73%,Al2O3含量15.65%~16.45%,Na2O/K2O值7.47~9.96,A/CNK为0.90~1.00,属中酸性岩系列,显示相对富钠、低钾的特征,A/CNK=0.90~1.00,属于准铝质低钾钙碱性系列;稀土总量较低(33.40×10-6~39.27×10-6),LREE/HREE值为3.95~6.51,在稀土元素配分图解上呈现出右倾特征;δEu值1.23~1.49之间,呈现Eu呈正异常特征;在微量元素原始地幔标准化图解上,显示富集Ba、Sr,亏损Nb、Ti、Yb高场强元素的特征。对车路沟岩体地质、地球化学特征与产出背景的全面分析,认为其为奥陶纪祁连洋持续向华北板块俯冲,诱使俯冲洋壳部分熔融形成的埃达克岩。

  • 加载中
  • 图 1  车路沟一带地质简图

    Figure 1. 

    图 2  车路沟岩体野外露头及显微照片(a,b英云闪长玢岩;c,d闪长玢岩)

    Figure 2. 

    图 3  车路沟岩体稀土元素配分模式(a)和微量元素原始地幔标准化蛛网图(b)

    Figure 3. 

    图 4  车路沟英云闪长玢岩中锆石CL图像及LA ICP-MS测点位置

    Figure 4. 

    图 5  车路沟岩体中LA ICP-MS锆石U-Pb年龄谐和图及加权平均年龄图

    Figure 5. 

    图 6  车路沟岩体Y/Sr-Y和A/MF-C/MF图解

    Figure 6. 

    图 7  车路沟岩体(Y+Nb)-Rb(a)和Y-Nb图解(b)

    Figure 7. 

    表 1  车路沟岩体主量元素(%)、微量元素(10-6)分析结果

    Table 1.  Analytical results of major elements (%) and trace elements (10-6) of the Chelugou rock mass

    下载: 导出CSV

    表 2  车路沟岩体中LA ICP-MS锆石U-Pb同位素测年结果

    Table 2.  Zircon LA ICP-MS U-Pb isotopic data of the Chelugou pluton

    下载: 导出CSV
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出版历程
收稿日期:  2018-11-28
修回日期:  2020-03-17
刊出日期:  2020-06-25

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