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    辽东半岛丹东地区中生代花岗岩锆石U-Pb年龄、Hf同位素特征及其地质意义

    张朋 赵岩 寇林林 沙德铭 毕中伟 杨凤超

    张朋, 赵岩, 寇林林, 沙德铭, 毕中伟, 杨凤超, 2019. 辽东半岛丹东地区中生代花岗岩锆石U-Pb年龄、Hf同位素特征及其地质意义. 地球科学, 44(10): 3297-3313. doi: 10.3799/dqkx.2019.129
    引用本文: 张朋, 赵岩, 寇林林, 沙德铭, 毕中伟, 杨凤超, 2019. 辽东半岛丹东地区中生代花岗岩锆石U-Pb年龄、Hf同位素特征及其地质意义. 地球科学, 44(10): 3297-3313. doi: 10.3799/dqkx.2019.129
    Zhang Peng, Zhao Yan, Kou Linlin, Sha Deming, Bi Zhongwei, Yang Fengchao, 2019. Zircon U-Pb Ages, Hf Isotopes and Geological Significance of Mesozoic Granites in Dandong Area, Liaodong Peninsula. Earth Science, 44(10): 3297-3313. doi: 10.3799/dqkx.2019.129
    Citation: Zhang Peng, Zhao Yan, Kou Linlin, Sha Deming, Bi Zhongwei, Yang Fengchao, 2019. Zircon U-Pb Ages, Hf Isotopes and Geological Significance of Mesozoic Granites in Dandong Area, Liaodong Peninsula. Earth Science, 44(10): 3297-3313. doi: 10.3799/dqkx.2019.129

    辽东半岛丹东地区中生代花岗岩锆石U-Pb年龄、Hf同位素特征及其地质意义

    doi: 10.3799/dqkx.2019.129
    基金项目: 

    国家重点研发计划 2016YFC0600108

    国家重点研发计划 2018YFC0603804

    中国地质调查局地质调查项目 DD20190165

    国家自然科学基金项目 41502093

    中国地质调查局地质调查项目 DD20190042-3

    中国地质调查局地质调查项目 DD20160049

    详细信息
      作者简介:

      张朋(1983—), 男, 工程师, 博士, 从事矿产地质调查及综合研究工作

    • 中图分类号: P581

    Zircon U-Pb Ages, Hf Isotopes and Geological Significance of Mesozoic Granites in Dandong Area, Liaodong Peninsula

    • 摘要: 为了确定辽东半岛丹东地区中生代花岗岩岩石类型、成岩时代及其形成构造背景.选取三股流岩体、五龙背岩体和丁岐山岩体开展岩相学、锆石LA-ICP-MS U-Pb年代学、岩石地球化学和锆石Hf同位素地球化学研究.结果表明:三股流岩体由花岗闪长岩、似斑状黑云母二长花岗岩和中粗粒黑云母二长花岗岩组成,后两者成岩年龄分别为137.2±1.2 Ma和123.2±1.3 Ma;丁岐山岩体由中细粒碱长花岗岩、石英正长岩和石英二长岩组成,获得中细粒碱长花岗岩成岩年龄为121.1±1.5 Ma;五龙背岩体由中粗粒二长花岗岩组成,成岩年龄为146.8±0.8 Ma.元素和同位素地球化学特征表明,三股流岩体的花岗闪长岩为钾玄岩系列,似斑状黑云母二长花岗岩和中粗粒黑云母二长花岗岩以及五龙背岩体和丁岐山岩体均为高钾钙碱性,3个岩体不同岩石类型的A/CNK均小于1.1,为I型花岗岩;岩体均富集轻稀土元素和大离子亲石元素,亏损重稀土元素和高场强元素,具Eu负异常;εHft)值为-22.40~-9.77,两阶段Hf模式年龄TDM2为2 999~1 915 Ma,揭示三股流岩体、五龙背岩体和丁岐山岩体可能是古元古代古老地壳部分熔融形成.结合区域构造演化认为三股流岩体、五龙背岩体和丁岐山岩体均形成于活动大陆边缘,五龙背岩体形成于古太平洋板块向欧亚板块的俯冲挤压的构造背景,三股流岩体和丁岐山岩体形成于古太平洋板块向欧亚板块的俯冲后的伸展环境.

       

    • 图  1  中国辽东半岛地质简图

      Zhang et al.(2016)

      Fig.  1.  Simplified geological map of Liaodong peninsula, China

      图  2  辽东丹东三股流岩体地质简图(a)和辽东丹东五龙背-丁岐山岩体地质简图(b)

      Fig.  2.  Simplified geological map of Sanguliu pluton (a) and Wulongbei-Dingqishan pluton (b), Dandong, Liaodong

      图  3  辽东半岛丹东地区花岗岩手标本和镜下照片

      a, b.三股流花岗闪长岩;c, d.三股流似斑状黑云二长花岗岩;e, f.三股流中粗粒黑云二长花岗岩;g, h.五龙背中粗粒黑云母花岗岩;i, j.丁岐山中细粒碱厂花岗岩. a, c, e, g, i为岩石标本照片;b, d, f, h, j为显微镜下正交偏光照片图中;Q.石英;Pl.斜长石;Or.钾长石、正长石;Bi.黑云母

      Fig.  3.  Photograghs and microscope photograghs for granite rocks in Dandong, Liaodong peninsula

      图  4  辽东半岛丹东地区花岗岩的SiO2-Na2O+K2O(a),SiO2-K2O(b)和A/CNK-A/NK(c)图解

      图a据Le Maitre et al.(1989); 图b据Rickwood(1989); 图c据Maniar and Piccoli(1989)

      Fig.  4.  Plots of SiO2-Na2O+K2O (a), SiO2-K2O (b) and A/CNK-A/NK(c) for granite rocks in Dandong, Liaodong peninsula

      图  5  辽东半岛丹东地区花岗岩的稀土配分曲线(a,c,e,g,i)和微量蛛网图(b,d,f,h)

      标准值据Sun and McDonough(1989)

      Fig.  5.  Rare earth element distribution curves (a, c, e, g, i) and trace element spider diagrams (b, d, f, h) for granite rocks in Dandong, Liaodong peninsula

      图  6  辽东半岛丹东地区花岗岩锆石阴极发光(CL)图像

      黑色圈为锆石U-Pb测定点;黄色点为Hf测试点

      Fig.  6.  Zircon CL images of granite rocks in Dandong, Liaodong peninsula

      图  7  辽东半岛丹东地区花岗岩锆石LA-ICP-MS U-Pb年龄谐和图和加权平均年龄图

      Fig.  7.  LA-ICP-MS U-Pb age of granite rocks in Dandong, Liaodong peninsula

      图  8  辽东半岛花岗岩的锆石Lu-Hf同位素特征图解

      Yang et al.(2006)

      Fig.  8.  Lu-Hf diagram of the granite rocks of Dingqishan rocks in Dandong, Liaodong peninsula

      图  9  丹东地区花岗岩成因类型判别图(Zr+Nb+Ce+Y)-(K2O+Na2O) (a); (Zr+Nb+Ce+Y)-(FeOT/MgO) (b); 10 000Ga/Al-Zr; (d) 10 000Ga/Al-Nb(c)

      FG.分异的I型、S型花岗岩分布区; OGT. I型、S型、M型花岗岩分布区;图a~d据Whalen et al.(1987)

      Fig.  9.  Granite genesis and type discrimination diagrams (Zr+Nb+Ce+Y)-(K2O+Na2O) (a), (Zr+Nb+Ce+Y)-(FeOT/MgO) (b), 10 000Ga/Al-Zr (c); 10 000Ga/Al-Nb(d)

      图  10  丹东地区花岗岩Rb /30-Hf-3Ta三元图解(a)和Rb-(Y+Nb)图解(b)

      图a据Harris et al.(1986);图b据Pearce et al.(1984)

      Fig.  10.  Rb/30-Hf-3Ta diagram(a); Rb-(Y+Nb) diagram(b)

      表  1  辽东半岛丹东地区花岗岩岩相学基本特征

      Table  1.   Petrographic features of granite rocks in Dandong, Liaodong peninsula

      岩石名称 采样位置 组构和矿物组成 备注
      三股流花岗闪长岩 124°13′42″E、40°06′14″N 中粗粒花岗结构,块状构造;粒度一般在3.5~6.0 mm, 个别2.5~3.0 mm;斜长石(50%)(An=36)、钾长石(20%)、石英(20%)、黑云母(5%)、角闪石(5%),副矿物为磷灰石、磁铁矿、锆石、褐帘石、榍石等 图 3a~3b
      三股流似斑状黑云母二长花岗岩 124°15′20″E、40°05′54″N 似斑状结构,基质为中粒花岗结构,块状构造;粒度一般在2.8~10.0 mm, 少量0.5~1.5 mm, 个别1.6~2.0 mm;斜长石(30%)(An=22)、钾长石(30%)、石英(25%)、黑云母(10%)、角闪石(5%),副矿物为磷灰石、磁铁矿、锆石、褐帘石、榍石等 图 3c~3d
      三股流中粗粒二长花岗岩 124°14′45″E、40°06′15″N 中粗粒花岗结构,块状构造;粒度一般在0.6~2.8 mm, 个别4.0~6.3 mm;斜长石(30%)(An=22)、钾长石(25%)、石英(30%)、黑云母(10%)、角闪石(5%),副矿物为磷灰石、磁铁矿、锆石、褐帘石、榍石等 图 3e~3f
      五龙背岩体中粗粒二长花岗岩 124°16′30″E、40°16′45″N 中粗粒花岗结构,块状构造;粒度一般在0.6~2.8 mm, 个别4.0~6.3 mm;斜长石(30%)、钾长石(35%)、石英(30%)、黑云母(5%),副矿物为磷灰石、锆石、褐帘石、榍石等 图 3g~3h
      丁岐山岩体中细粒碱长花岗岩 124°21′49″E、40°17′29″N 中细粒花岗结构,块状构造;粒度一般在0.3~0.6 mm, 少量0.7~0.8 mm, 个别3~5 mm以上;条纹长石(55%)、斜长石(5%)(An=15±)、石英(30%)、黑云母(5%),副矿物为磷灰石、锆石、磁铁矿、榍石等 图 3i~3j
      下载: 导出CSV
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