柴北缘构造带欧龙布鲁克地块西北缘辉长岩脉地球化学、年代学及Hf同位素特征

庄玉军, 辜平阳, 李培庆, 何世平, 陈锐明, 查显锋. 柴北缘构造带欧龙布鲁克地块西北缘辉长岩脉地球化学、年代学及Hf同位素特征[J]. 地质通报, 2019, 38(11): 1801-1812.
引用本文: 庄玉军, 辜平阳, 李培庆, 何世平, 陈锐明, 查显锋. 柴北缘构造带欧龙布鲁克地块西北缘辉长岩脉地球化学、年代学及Hf同位素特征[J]. 地质通报, 2019, 38(11): 1801-1812.
ZHUANG Yujun, GU Pingyang, LI Peiqing, HE Shiping, CHEN Ruiming, ZHA Xianfeng. Geochemistry, geochronology and Hf isotopic compositions of metagabbro dykes on the northwestern margin of Oulongbuluke micro-block on the northern margin of Qaidam Basin[J]. Geological Bulletin of China, 2019, 38(11): 1801-1812.
Citation: ZHUANG Yujun, GU Pingyang, LI Peiqing, HE Shiping, CHEN Ruiming, ZHA Xianfeng. Geochemistry, geochronology and Hf isotopic compositions of metagabbro dykes on the northwestern margin of Oulongbuluke micro-block on the northern margin of Qaidam Basin[J]. Geological Bulletin of China, 2019, 38(11): 1801-1812.

柴北缘构造带欧龙布鲁克地块西北缘辉长岩脉地球化学、年代学及Hf同位素特征

  • 基金项目:
    陕西自然科学基金项目《青海阿尔金东段新太古代米兰岩群中麻粒岩成因及变质作用过程研究》(编号:2017JM4001)、国家自然科学基金项目《青藏高原羌塘地区地壳早期物质探索研究》(批准号:41002063)和中国地质调查局项目《商丹-大柴旦地区区域地质调查》(编号:DD20190069)
详细信息
    作者简介: 庄玉军(1989-), 男, 硕士, 工程师, 地质工程专业。E-mail:zhuangyujun@126.com
    通讯作者: 辜平阳(1982-), 男, 博士, 高级工程师, 矿物、岩石、矿床学专业。E-mail:pingyang-322@163.com
  • 中图分类号: P597+.3;P588.12

Geochemistry, geochronology and Hf isotopic compositions of metagabbro dykes on the northwestern margin of Oulongbuluke micro-block on the northern margin of Qaidam Basin

More Information
  • 侵位于柴北缘构造带欧龙布鲁克地块西北缘达肯大坂岩群中的辉长岩脉岩石Al2O3、CaO含量较高,P2O5、TiO2含量较低,属于钙碱性系列。稀土元素总量低(43.17×10-6~57.53×10-6),LREE/HREE值为1.82~2.77,稀土元素配分曲线整体表现为右倾型。岩石Ti亏损,具高ThN/NbN值(3.75~8.03)和低Nb/La值(0.44~0.84)特征。辉长岩锆石的176Hf/177Hf值介于0.282813~0.282979之间,εHft)值为9.25~15.11,Hf模式年龄(TDM)分布在378~610Ma之间,平均494Ma。综合研究认为,辉长岩岩浆源区为软流圈地幔且后期可能受到壳源富集组分的混染。LA-ICP-MS锆石U-Pb定年结果表明,辉长岩脉形成于357±4Ma,即早石炭世。结合区域地质背景,认为早石炭世柴北缘仍处于后造山伸展的构造演化阶段,而辉长岩脉是后造山伸展阶段柴北缘造山带去根、软流圈地幔上涌作用形成的。

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  • 图 1  柴北缘地质简图(a,底图据参考文献[26]修改)及研究区地质图(b)

    Figure 1. 

    图 2  辉长岩岩相学特征

    Figure 2. 

    图 3  辉长岩Nb/Y-Zr/TiO2×0.0001图

    Figure 3. 

    图 4  辉长岩AFM图解

    Figure 4. 

    图 5  辉长岩稀土元素球粒陨石标准化图解(a)和微量元素原始地幔标准化蛛网图(b)[37]

    Figure 5. 

    图 6  辉长岩代表性锆石阴极发光图像

    Figure 6. 

    图 7  辉长岩锆石U-Pb谐和图(a)和206Pb/238U年龄加权平均值(b)

    Figure 7. 

    图 8  辉长岩锆石年龄-εHft)图解(底图据参考文献[45])

    Figure 8. 

    图 9  辉长岩ThN/NbN-Nb/La图解(底图据参考文献[48])

    Figure 9. 

    表 1  辉长岩主量、微量及稀土元素含量分析结果

    Table 1.  Major, trace elements and REE compositions of metagabbro

    下载: 导出CSV

    表 2  辉长岩LA-ICP-MS锆石U-Th-Pb同位素测年结果

    Table 2.  LA-ICP-MS zircon U-Th-Pb isotopic analyses of metagabbro

    下载: 导出CSV

    表 3  变辉长岩锆石Hf同位素组成

    Table 3.  Zircon Hf isotope compositions of metagabbro

    下载: 导出CSV
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    辜平阳,董增产,陈锐明,等.青海阿尔金1:5万打柴沟(J46E005011、J46E005012、J46E005013、J46E006011、J46E006012、J46E006013)等6幅区调.2016.

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收稿日期:  2018-05-17
修回日期:  2018-07-03
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