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    东昆仑祁漫塔格阿确墩地区侵入岩U-Pb年代学、地球化学及其地质意义

    李婷 李猛 胡朝斌 李瑶 孟杰 高晓峰 查显锋

    李婷, 李猛, 胡朝斌, 李瑶, 孟杰, 高晓峰, 查显锋, 2018. 东昆仑祁漫塔格阿确墩地区侵入岩U-Pb年代学、地球化学及其地质意义. 地球科学, 43(12): 4350-4363. doi: 10.3799/dqkx.2018.224
    引用本文: 李婷, 李猛, 胡朝斌, 李瑶, 孟杰, 高晓峰, 查显锋, 2018. 东昆仑祁漫塔格阿确墩地区侵入岩U-Pb年代学、地球化学及其地质意义. 地球科学, 43(12): 4350-4363. doi: 10.3799/dqkx.2018.224
    Li Ting, Li Meng, Hu Chaobin, Li Yao, Meng Jie, Gao Xiaofeng, Zha Xianfeng, 2018. Zircon U-Pb Geochronology, Geochemistry and Its Geological Implications of Intrusions in Aquedun Area from Qimantag, East Kunlun, China. Earth Science, 43(12): 4350-4363. doi: 10.3799/dqkx.2018.224
    Citation: Li Ting, Li Meng, Hu Chaobin, Li Yao, Meng Jie, Gao Xiaofeng, Zha Xianfeng, 2018. Zircon U-Pb Geochronology, Geochemistry and Its Geological Implications of Intrusions in Aquedun Area from Qimantag, East Kunlun, China. Earth Science, 43(12): 4350-4363. doi: 10.3799/dqkx.2018.224

    东昆仑祁漫塔格阿确墩地区侵入岩U-Pb年代学、地球化学及其地质意义

    doi: 10.3799/dqkx.2018.224
    基金项目: 

    中国地质调查局项目 DD20160002

    详细信息
      作者简介:

      李婷(1984-), 女, 硕士, 工程师, 矿物学、岩石学、矿床学专业

    • 中图分类号: P581

    Zircon U-Pb Geochronology, Geochemistry and Its Geological Implications of Intrusions in Aquedun Area from Qimantag, East Kunlun, China

    • 摘要: 祁漫塔格地区岩浆岩的成岩时代和形成环境的确定能对东昆仑造山带加里东期构造演化时限加以约束.对祁漫塔格西北部阿确墩地区石英闪长岩和二长花岗岩进行了年代学和岩石地球化学研究,结果显示,石英闪长岩属准铝质-弱过铝质钙碱性系列岩石;轻重稀土分馏明显,具中等-轻微铕负异常(δEu=0.79~0.90);相对富集Rb、K、Hf、Zr、Tb、Nd等元素,不同程度地亏损Ba、P、Ti、Nd、Ta、Y;具有I型花岗岩类特征.二长花岗岩属弱过铝质钙碱性系列岩石;轻重稀土分异程度极大,具明显铕负异常(δEu=0.42~0.45);富集大离子亲石元素(如Rb、K、La、Ce、Nd、Tb等),亏损高场强元素(P、Ti、Nd、Ta)和Ba、Sr、U等元素;为高分异I型花岗岩.Nd/Th、Nb/Ta、Mg#值等指标显示石英闪长岩为壳源特征且受到幔源岩浆的影响,推测是幔源岩浆底侵地壳物质发生部分熔融形成的;二长花岗岩则是壳源的,可能与幔源岩浆底侵诱发的上地壳物质部分熔融有关,且经历了强烈的结晶分离作用.石英闪长岩和二长花岗岩的LA-ICP-MS锆石U-Pb年龄分别为448.8±3.9 Ma和405.2±3.6 Ma,代表其形成时代.石英闪长岩总体显示出与俯冲消减作用有关的岛弧岩浆岩地球化学特征;二长花岗岩在构造环境图解中显示为碰撞背景,但微量元素与同碰撞花岗岩典型特征不符,综合分析认为形成于后碰撞构造背景下.结合区域构造演化,推测东昆仑祁漫塔格地区在晚奥陶世持续处于俯冲消减环境中,早泥盆世之前进入后碰撞造山阶段.

       

    • 图  1  东昆仑阿确墩地区地质简图

      Fig.  1.  The sketch geological map of the Aquedun area in the East Kunlun orogen

      图  2  东昆仑阿确墩地区岩体主量元素判别图解

      a.据Middlemost(1994)清绘;b.岩石类型边界引自Rickwood(1989)

      Fig.  2.  Major element diagrams of intrusions in Aquedun area in the East Kunlun orogen

      图  3  东昆仑阿确墩地区岩体REE球粒陨石标准化配分型式(a)和微量元素原始地幔标准化蛛网图(b)

      球粒陨石和原始地幔标准化值据Sun and McDonough(1989)

      Fig.  3.  Chondrite-normalized REE pattern (a) and primitive mantle-normalized trace element pattern (b) of intrusions in Aquedun area in the East Kunlun orogen

      图  4  东昆仑阿确墩地区岩体锆石CL图像

      Fig.  4.  CL images of zircons of intrusions in Aquedun area in the East Kunlun orogen

      图  5  东昆仑阿确墩地区岩体LA-ICP-MS锆石U-Pb年龄谐和图和表面加权平均年龄图

      Fig.  5.  LA-ICP-MS zircon U-Pb condordia diagrams and weighted average ages of intrusions in Aquedun area in the East Kunlun orogen

      图  6  东昆仑阿确墩地区岩体地球化学图解

      FG.分异的M、I、S型花岗岩;OGT.未分异的M、I、S型花岗岩

      Fig.  6.  Diagrams of intrusions in Aquedun area in the East Kunlun orogen

      图  7  东昆仑阿确墩地区岩体Nb-Nb/Ta图解

      Barth et al.(2000)

      Fig.  7.  Nb-Nb/Ta diagram of intrusions in Aquedun area in the East Kunlun orogen

      图  8  东昆仑阿确墩地区岩体Sr-Ba图解

      Li et al.(2007);PlAn50.斜长石(An=50);PlAn15.斜长石(An=15);Kfs.钾长石;Amp.角闪石;Grt.石榴石;Ms.白云母;Bt.黑云母

      Fig.  8.  Sr-Ba diagram of intrusions in Aquedun area in the East Kunlun orogen

      图  9  东昆仑阿确墩地区岩体构造环境判别图

      1.地幔斜长岩幔源花岗岩;2.钙碱性更长花岗岩-板块碰撞前消减地区花岗岩;3.高钾钙碱性花岗岩-板块碰撞后隆起区花岗岩;4.造山晚期-晚造山期花岗岩(二长岩);5.非造山期A型花岗岩;6.同碰撞花岗岩(S型);7.造山后期A型花岗岩.a、c.据Pearce et al.(1984);b.据Harris et al.(1986)

      Fig.  9.  Tectonic setting discrimination diagrams of intrusions in Aquedun area in the East Kunlun orogen

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    • 收稿日期:  2018-06-29
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