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    扬子板块西北缘大安花岗岩体锆石U-Pb年代学、地球化学特征及其地质意义

    栗朋 裴先治 李瑞保 李佐臣 杨运军 陈有炘 刘成军 王盟 裴磊 高峰 苏朕国 梁国冰 高翔宇

    栗朋, 裴先治, 李瑞保, 李佐臣, 杨运军, 陈有炘, 刘成军, 王盟, 裴磊, 高峰, 苏朕国, 梁国冰, 高翔宇, 2019. 扬子板块西北缘大安花岗岩体锆石U-Pb年代学、地球化学特征及其地质意义. 地球科学, 44(4): 1338-1356. doi: 10.3799/dqkx.2018.163
    引用本文: 栗朋, 裴先治, 李瑞保, 李佐臣, 杨运军, 陈有炘, 刘成军, 王盟, 裴磊, 高峰, 苏朕国, 梁国冰, 高翔宇, 2019. 扬子板块西北缘大安花岗岩体锆石U-Pb年代学、地球化学特征及其地质意义. 地球科学, 44(4): 1338-1356. doi: 10.3799/dqkx.2018.163
    Li Peng, Pei Xianzhi, Li Ruibao, Li Zuochen, Yang Yunjun, Chen Youxin, Liu Chengjun, Wang Meng, Pei Lei, Gao Feng, Su Zhenguo, Liang Guobing, Gao Xiangyu, 2019. Zircon U-Pb Geochronology, Geochemistry and Geological Significance of Daan Granite in Northwestern Margin of Yangtze Block. Earth Science, 44(4): 1338-1356. doi: 10.3799/dqkx.2018.163
    Citation: Li Peng, Pei Xianzhi, Li Ruibao, Li Zuochen, Yang Yunjun, Chen Youxin, Liu Chengjun, Wang Meng, Pei Lei, Gao Feng, Su Zhenguo, Liang Guobing, Gao Xiangyu, 2019. Zircon U-Pb Geochronology, Geochemistry and Geological Significance of Daan Granite in Northwestern Margin of Yangtze Block. Earth Science, 44(4): 1338-1356. doi: 10.3799/dqkx.2018.163

    扬子板块西北缘大安花岗岩体锆石U-Pb年代学、地球化学特征及其地质意义

    doi: 10.3799/dqkx.2018.163
    基金项目: 

    国家自然科学基金项目 40972136

    国家自然科学基金项目 41172186

    国家自然科学基金项目 41502191

    中央高校基本科研业务费专项资金项目 310827161006

    国家自然科学基金项目 41872233

    陕西省公益性基础地质调查专项"陕西省勉略宁地区基础地质调查" 20150102

    国家自然科学基金项目 41472191

    中央高校基本科研业务费专项资金项目 310827161002

    详细信息
      作者简介:

      栗朋(1994-), 男, 硕士研究生, 构造地质学专业

      通讯作者:

      裴先治

    • 中图分类号: P597

    Zircon U-Pb Geochronology, Geochemistry and Geological Significance of Daan Granite in Northwestern Margin of Yangtze Block

    • 摘要: 位于扬子板块西北缘宁强地区的大安花岗岩体,岩石类型主要为黑云母花岗闪长岩,但其形成时代却有一定的争议,成因及地质意义尚未明确.对大安花岗岩体进行详细的LA-ICP-MS锆石U-Pb年代学和岩石地球化学研究.结果表明,花岗闪长岩年龄为212.3±1.6 Ma和212.48±0.43 Ma,属晚三叠世.地球化学特征显示花岗闪长岩相对高硅(67.61%~69.02%)、高Al2O3(16.14%~16.80%),Na2O > K2O,富集大离子亲石元素(Cs、Ba)和轻稀土元素,Eu负异常不明显,强烈富集Sr(538×10-6~907×10-6)和亏损Y(3.10×10-6~3.90×10-6),高Sr/Y比值(138~291),表现出明显的埃达克质岩石的地球化学特征.综合区域地质资料认为,大安花岗岩体形成于后碰撞构造环境,是在华北板块与扬子板块碰撞后期伸展体制下,由于地幔物质上涌带来的热量导致加厚基性下地壳脱水熔融,形成了具有埃达克质性质的岩浆.

       

    • 图  1  大安花岗岩体构造位置及岩体地质简图

      1.第四系;2.志留系茂县群;3.上震旦统灯影组;4.下震旦统陡山沱组;5.下南华统莲沱组;6.新元古界碧口岩群;7.大安花岗岩体;8.断层;9.产状;10.采样位置.据陕西省地质调查中心, 2017, 1:5万陕西省勉略宁地区地质图

      Fig.  1.  Regional location map and geological map of Daan granite

      图  2  大安花岗岩体野外露头及显微镜下照片

      a, c, d.黑云母花岗闪长岩;b.大安花岗岩体(γδT)与志留系茂县群(SM)侵入接触,岩体中可见围岩捕掳体.矿物名称缩写:Pl.斜长石;Qtz.石英;Bi.黑云母;Ap.磷灰石

      Fig.  2.  Field and microscopic photos of Daan granite

      图  3  大安花岗岩体中粒黑云母花岗闪长岩(DA01/2)(a)和中粗粒黑云母花岗闪长岩(DA06/1)(b)代表性单颗粒锆石阴极发光图像和年龄值

      Fig.  3.  CL images and age values of selected zircons for biotite granodiorite (DA01/2) (a) and middle-coarse biotite granodiorite (DA06/1) (b) of the Daan granite

      图  4  大安花岗岩体中粒黑云母花岗闪长岩(DA01/2)(a, b)和中粗粒黑云母花岗闪长岩(DA06/1)(c, d)锆石U-Pb年龄谐和图

      Fig.  4.  U-Pb concordia diagrams of zircon for biotite granodiorite (DA01/2) (a, b) and middle-coarse biotite granodiorite (DA06/1) (c, d) of the Daan granite

      图  5  大安花岗岩体TAS(a)、K2O-Na2O(b)、SiO2-K2O(c) and A/NK-A/CNK(d)图解

      图a据Rickwood(1989),图b据Maniar and Piccoli(1989),虚线代表Ⅰ型和S型花岗岩之间的边界(Chappell and White, 1992)

      Fig.  5.  TAS (a), K2O-Na2O (b), SiO2-K2O (c) and A/NK-A/CNK (d) diagrams for Daan granite

      图  6  大安花岗岩体主要氧化物、微量元素Harker图解

      Fig.  6.  Harker plots of selected major and trace elements for the Daan granite

      图  7  大安花岗岩体稀土元素球粒陨石标准化配分曲线图(a)和微量元素原始地幔标准化蛛网图(b)

      球粒陨石标准化数据值引自Boynton(1984); 原始地幔标准化数据值引自Sun and McDonough(1989).埃达克岩据张旗等(2001)

      Fig.  7.  Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element spider diagram (b) for Daan granite

      图  8  大安花岗岩体Sr/Y-Y图解(a)和Sr-Yb图解(b)

      图a据Defant et al.(2002); 图b据张旗等(2008);Ⅰ.埃达克岩;Ⅱ.喜马拉雅型花岗岩;Ⅲ.广西型花岗岩;Ⅳ.南岭型花岗岩

      Fig.  8.  Sr/Y-Y (a) and Sr-Yb (b) diagrams of Daan granite

      图  9  大安花岗岩体岩石化学成分与变泥质岩、变杂砂岩、变角闪岩派生的实验熔体化学成分对比(a)和YbN-(La/Yb)N图解(b)

      图a据Kaygusuz et al.(2008); 图b据Drummond and Defant(1990)

      Fig.  9.  Chemical content contrast between Daan granite and meta-mudstone-, greywacke-, meta-amphibolite-derived experimental melt (a) and YbN-(La/Yb)N diagram(b) of Daan granite

      图  10  大安花岗岩体SiO2-lg[CaO/(K2O+Na2O)]图解(a)和R1-R2图解(b)

      图a据Brown and Nordin(1982);图b据Batchelor and Bowden(1985)

      Fig.  10.  SiO2-lg[CaO/(K2O+Na2O)] diagram (a) and R1-R2 diagram (b) of Daan granite

      表  1  大安花岗岩体与典型埃达克岩地球化学特征对比

      Table  1.   Comparison of geochemical characteristics of Daan granite and adakites

      典型埃达克岩 大安花岗岩体
      SiO2(%) >56 68.20
      Al2O3(%) >15 16.43
      K2O/Na2O <0.5 0.26
      Sr(10-6) >400 766
      Yb(10-6) <2 0.33
      Y(10-6) ≤18 3.55
      Mg# >47 35.66
      Sr/Y >40 218
      Zr/Sm >50 93
      La/Yb >20 12.54
      Eu异常 无Eu异常或Eu负异常不明显 弱负异常
      Sr异常
      注:据张旗等(2001).
      下载: 导出CSV
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