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    东乌旗晚石炭世辉石橄榄岩锆石U-Pb年龄及其构造意义

    程银行 张夏炜 王少轶 奥琮 李影 张天福 滕学建

    程银行, 张夏炜, 王少轶, 奥琮, 李影, 张天福, 滕学建, 2020. 东乌旗晚石炭世辉石橄榄岩锆石U-Pb年龄及其构造意义. 地球科学, 45(3): 844-855. doi: 10.3799/dqkx.2020.006
    引用本文: 程银行, 张夏炜, 王少轶, 奥琮, 李影, 张天福, 滕学建, 2020. 东乌旗晚石炭世辉石橄榄岩锆石U-Pb年龄及其构造意义. 地球科学, 45(3): 844-855. doi: 10.3799/dqkx.2020.006
    Cheng Yinhang, Zhang Xiawei, Wang Shaoyi, Ao Cong, Li Ying, Zhang Tianfu, Teng Xuejian, 2020. Zircon U-Pb Dating and Geochemistry of Late Carboniferous Pyroxene Peridotite in Dong Ujimqi Inner Mongolia and Its Tectonic Significance. Earth Science, 45(3): 844-855. doi: 10.3799/dqkx.2020.006
    Citation: Cheng Yinhang, Zhang Xiawei, Wang Shaoyi, Ao Cong, Li Ying, Zhang Tianfu, Teng Xuejian, 2020. Zircon U-Pb Dating and Geochemistry of Late Carboniferous Pyroxene Peridotite in Dong Ujimqi Inner Mongolia and Its Tectonic Significance. Earth Science, 45(3): 844-855. doi: 10.3799/dqkx.2020.006

    东乌旗晚石炭世辉石橄榄岩锆石U-Pb年龄及其构造意义

    doi: 10.3799/dqkx.2020.006
    基金项目: 

    国家自然科学基金面上项目 41872068

    中国地质调查局项目 1212011220446

    中国地质调查局项目 1212011120697

    详细信息
      作者简介:

      程银行(1982-), 男, 副研究员, 博士, 从事地质矿产调查与研究工作

    • 中图分类号: P581

    Zircon U-Pb Dating and Geochemistry of Late Carboniferous Pyroxene Peridotite in Dong Ujimqi Inner Mongolia and Its Tectonic Significance

    • 摘要: 目前关于内蒙古东乌旗晚古生代花岗岩中辉石橄榄包体的精确年代学及其构造意义不清,直接制约了该区晚古生代地幔性质及构造演化的探讨.对东乌旗新发现的辉石橄榄岩进行了岩相学、全岩地球化学和锆石U-Pb定年研究.结果表明,辉石橄榄岩主要由橄榄石、角闪石、斜方辉石及少量斜长石、黑云母、单斜辉石组成;锆石U-Pb年龄为317.8±1.6 Ma,属晚石炭世.地球化学数据显示,岩石SiO2含量为40.28%~44.50%、MgO含量为23.42%~29.44%、Na2O+K2O含量为1.00%~2.12%(小于3.5%),具有低m/f比值(3.13~3.86)和高FeOT含量(11.18%~14.70%)、高Mg#值(75.60~79.26),属铁质超镁铁岩和拉斑玄武岩系列.岩石稀土总量较高(∑REE=31.98×10-6~72.60×10-6),轻稀土(LREE)相对于重稀土(HREE)富集,(La/Yb)N=3.56~7.72,Eu异常不明显(δEu=0.79~1.65),球粒陨石标准化稀土元素配分模式表现为右倾型.岩石富集大离子亲石元素Rb、Sr、K等,相对亏损高场强元素Nb、Ta,具明显的Nb、Ta、Ti负异常;其形成于受俯冲流体改造的岩石圈地幔的减薄作用,并且岩浆在演化过程中遭受了地壳物质的同化混染作用.

       

    • 图  1  中亚造山带(a)、兴蒙造山带(b)构造简图和内蒙古东乌旗西部地质简图(c)

      Cheng et al.(2014)修改. TC.塔里木板块;NCC.华北板块.除317.8±1.6 Ma外,其他年龄数据均来源于Cheng et al.(2014)

      Fig.  1.  Geological sketch maps of Central-Asian Orogenic Belt (a) and Xing'an-Mongolian Orogenic Belt (b) and western Dong Ujimqi, Inner Mongolia (c)

      图  2  内蒙古东乌旗辉石橄榄岩野外宏观(a~d)和偏光显微照片(e、f)

      Ol.橄榄石;Opx.斜方辉石;Pl.斜长石;Hb.角闪石

      Fig.  2.  Macro photos (a-d) and photomicrographs (e, f) of pyroxene peridotite in Dong Ujimqi, Inner Mongolia

      图  3  内蒙古东乌旗辉石橄榄岩样品(7217)的部分锆石阴极发光图像

      Fig.  3.  CL images of selected zircons of the pyroxene peridotite sample (7217) in Dong Ujimqi, Inner Mongolia

      图  4  内蒙古东乌旗辉石橄榄岩锆石U-Pb年龄谐和图

      Fig.  4.  Zircon U-Pb concordia diagram of the pyroxene peridotite in Dong Ujimqi, Inner Mongolia

      图  5  内蒙古东乌旗辉石橄榄岩稀土元素球粒陨石标准化配分模式(a)和原始地幔标准化微量元素蛛网图(b)

      Sun and McDonough(1989)

      Fig.  5.  Chondrite-normalized REE pattern(a)and primitive mantle-normalized trace element spider diagram(b)of the pyroxene peridotite in Dong Ujimqi, Inner Mongolia

      图  6  内蒙古东乌旗辉石橄榄岩的部分熔融判别图解

      图a据程银行等(2016);图b据Onuma et al.(1981).实心和空心分别代表稀土总量高和稀土总量低的辉石橄榄岩

      Fig.  6.  Discrimination diagrams of partial melting of the pyroxene peridotite in Dong Ujimqi, Inner Mongolia

      图  7  内蒙古东乌旗辉石橄榄岩的地幔岩相判别图

      图a据Münker(2000);图b据Deniel(1998).实心和空心分别代表稀土总量高和稀土总量低的辉石橄榄岩

      Fig.  7.  Discrimination diagrams of pyrolite phase of the pyroxene peridotite in Dong Ujimqi, Inner Mongolia

      图  8  内蒙古东乌旗辉石橄榄岩的Zr/4-2Nb-Y图解

      Meschede(1986). A1.板内碱性玄武岩;A2.板内玄武岩和板内拉斑玄武岩;B.E-MORB;C.板内拉斑玄武岩和火山弧玄武岩;D. N-MORB和火山弧玄武岩.实心和空心分别代表稀土总量高和稀土总量低的辉石橄榄岩

      Fig.  8.  Zr/4-2Nb-Y diagram of the pyroxene peridotite in Dong Ujimqi, Inner Mongolia

      表  1  内蒙古东乌旗辉石橄榄岩LA-MC-ICP-MS锆石U-Pb同位素分析结果

      Table  1.   Zircon LA-MC-ICP-MS U-Pb dating result of pyroxene peridotite in Dong Ujimqi, Inner Mongolia

      测点号 元素含量及比值 同位素比值 年龄(Ma)
      U(10-6) Th(10-6) Th/U 206Pb/ 238U ±1σ 207Pb/ 235U ±1σ 207Pb/ 206Pb ±1σ 206Pb/ 238U ±1σ 207Pb/ 235U ±1σ
      7217.1 521 683 1.31 0.050 2 0.000 6 0.362 0 0.006 0 0.052 3 0.000 7 316 4 314 5
      7217.2 92 67 0.72 0.050 9 0.000 6 0.369 7 0.023 7 0.052 6 0.003 3 320 4 319 21
      7217.3 400 609 1.52 0.051 0 0.000 6 0.370 5 0.008 9 0.052 7 0.000 9 320 4 320 8
      7217.4 342 184 0.54 0.050 6 0.000 9 0.367 6 0.010 8 0.052 7 0.001 4 318 6 318 9
      7217.5 188 222 1.18 0.050 4 0.000 6 0.365 1 0.009 2 0.052 5 0.001 2 317 4 316 8
      7217.6 166 124 0.75 0.050 4 0.000 6 0.365 8 0.010 6 0.052 6 0.001 4 317 4 317 9
      7217.7 227 165 0.73 0.050 5 0.000 6 0.366 2 0.008 1 0.052 6 0.001 1 317 4 317 7
      7217.8 175 213 1.22 0.051 1 0.000 6 0.371 9 0.008 0 0.052 8 0.001 1 321 4 321 7
      7217.9 811 610 0.75 0.050 2 0.000 6 0.365 1 0.005 6 0.052 7 0.000 6 316 4 316 5
      7217.10 521 625 1.20 0.050 2 0.000 6 0.368 4 0.006 1 0.053 2 0.000 7 316 4 318 5
      7217.11 367 314 0.85 0.050 8 0.000 6 0.369 6 0.007 0 0.052 8 0.001 0 319 3 319 6
      7217.12 534 612 1.15 0.050 6 0.000 6 0.369 0 0.006 0 0.052 9 0.000 7 318 4 319 5
      7217.13 2 052 2730 1.33 0.050 5 0.000 6 0.367 0 0.005 2 0.052 7 0.000 6 318 4 317 4
      7217.14 749 633 0.84 0.050 5 0.000 6 0.367 7 0.006 1 0.052 8 0.000 8 318 4 318 5
      7217.15 764 803 1.05 0.050 9 0.000 6 0.369 9 0.007 3 0.052 7 0.000 8 320 4 320 6
      7217.16 247 246 0.99 0.050 3 0.000 6 0.366 2 0.012 0 0.052 8 0.001 7 317 4 317 10
      7217.17 428 597 1.39 0.050 6 0.000 6 0.369 8 0.006 3 0.053 0 0.000 9 318 4 319 5
      7217.18 645 1 175 1.82 0.050 6 0.000 6 0.369 2 0.007 0 0.052 9 0.000 8 318 4 319 6
      7217.19 491 7 0.02 0.050 6 0.000 8 0.367 7 0.008 4 0.052 7 0.001 0 318 5 318 7
      7217.20 92 63 0.68 0.049 8 0.000 6 0.363 6 0.023 3 0.053 0 0.003 3 313 4 315 20
      7217.21 497 12 0.03 0.050 5 0.000 6 0.369 1 0.009 2 0.053 0 0.001 4 318 4 319 8
      7217.24 710 6 0.01 0.050 9 0.001 2 0.370 4 0.010 4 0.052 8 0.000 8 320 8 320 9
      下载: 导出CSV

      表  2  内蒙古东乌旗辉石橄榄岩主量元素(%)和微量元素(10-6)分析结果

      Table  2.   Major element (%) and trace element (10-6) contents of pyroxene peridotite in Dong Ujimqi, Inner Mongolia

      编号 7216-4 7216-5 7216-6 7217 P19-13-4 P19-13-5 P19-13-6
      SiO2 43.57 44.50 43.88 40.28 43.00 43.33 43.02
      Al2O3 7.93 7.94 7.96 5.67 7.73 7.56 7.59
      Fe2O3 3.81 3.67 3.34 4.90 2.83 3.99 3.08
      FeO 8.16 8.08 8.18 10.29 11.29 10.42 11.16
      CaO 6.70 6.58 6.54 3.27 3.70 3.75 3.62
      MgO 23.99 23.42 23.96 29.44 24.92 24.33 25.22
      K2O 0.42 0.40 0.40 0.44 0.88 1.05 0.90
      Na2O 1.06 1.04 1.04 0.56 1.12 1.07 1.08
      TiO2 0.42 0.44 0.43 0.26 0.84 0.86 0.82
      P2O5 0.08 0.08 0.07 0.08 0.24 0.25 0.25
      MnO 0.19 0.18 0.18 0.23 0.21 0.21 0.21
      LOI 2.77 2.77 3.10 3.44 1.99 2.02 1.79
      总量 99.09 99.09 99.08 98.86 98.75 98.84 98.74
      Mg# 78.70 78.60 79.26 78.14 76.27 75.60 76.36
      FeOT 11.59 11.38 11.18 14.70 13.84 14.01 13.93
      m/f 3.73 3.70 3.86 3.61 3.24 3.13 3.26
      K2O+Na2O 1.48 1.44 1.44 1.00 2.00 2.12 1.98
      K2O/Na2O 0.39 0.38 0.38 0.78 0.78 0.98 0.83
      K2O/TiO2 1.00 0.90 0.93 1.69 1.04 1.22 1.09
      P2O5 /Al2O3 0.01 0.01 0.01 0.01 0.03 0.03 0.03
      Cu 13.8 20.0 16.8 8.9 70.1 62.8 62.6
      Pb 8.83 6.98 7.98 58.80 4.12 4.25 4.08
      Zn 93.8 93.9 91.6 136 119 121 119
      Cr 1 290 1 230 1 260 728 1 510 1 460 1 530
      Ni 413 399 398 586 842 831 880
      Co 97.8 94.8 95.6 132 107 106 111
      Li 9.5 10.2 10.3 13.8 28.9 33.2 31.8
      Rb 11.9 11.8 11.0 18.5 36.5 48.1 40.6
      Cs 2.62 2.54 2.24 7.11 21.10 26.40 24.00
      Sr 370 362 362 177 347 255 359
      Ba 79.9 92.4 93.2 79.2 159 143 170
      V 96.2 96.3 96.2 77.8 124 123 125
      Sc 20.4 17.5 20.0 9.0 10.9 12.4 12.4
      Nb 1.49 1.57 1.48 1.43 3.31 3.28 3.34
      Ta 0.12 0.12 0.10 0.14 0.21 0.22 0.22
      Zr 38.3 41.0 37.4 42.0 99.3 101 105
      Hf 1.22 1.27 1.22 1.16 2.64 2.70 2.82
      Ga 8.6 8.33 8.72 6.33 9.96 9.83 10.6
      U 0.41 0.39 0.42 0.78 0.29 0.32 0.32
      Th 1.25 1.21 1.33 1.72 0.76 0.83 1.66
      La 5.26 5.24 6.44 5.84 9.20 9.25 10.80
      Ce 12.0 12.0 14.2 12.6 22.6 22.7 26.1
      Pr 1.67 1.67 1.92 1.64 3.34 3.35 3.79
      Nd 7.34 7.43 8.36 6.7 15.2 15.3 17.2
      Sm 1.67 1.70 1.88 1.40 3.50 3.51 3.87
      Eu 0.52 0.53 0.56 0.36 1.03 1.03 1.08
      Gd \ \ \ 1.32 \ \ \
      Tb 0.25 0.26 0.28 0.20 0.54 0.56 0.63
      Dy 1.40 1.53 1.58 1.00 3.00 3.15 3.65
      Ho 0.27 0.28 0.30 0.20 0.60 0.61 0.74
      Er 0.74 0.76 0.84 0.55 1.64 1.65 2.06
      Tm 0.10 0.11 0.12 0.081 0.23 0.24 0.32
      Yb 0.66 0.70 0.77 0.51 1.47 1.56 2.04
      Lu 0.10 0.11 0.12 0.08 0.23 0.24 0.32
      Y 6.74 6.79 7.42 5.08 14.50 14.60 17.90
      ΣREE 31.98 32.32 37.37 32.48 62.58 63.15 72.60
      (La/Sm)N 1.98 1.93 2.15 2.62 1.65 1.65 1.75
      (La/Yb)N 5.37 5.04 5.63 7.72 4.21 3.99 3.56
      δEu 1.65 1.65 1.58 0.79 1.56 1.55 1.48
      Rb/Sr 0.03 0.03 0.03 0.10 0.11 0.19 0.11
      注:Mg#=100×Mg2+/(Mg2++Fe2+);FeOT=FeO+0.899 8Fe2O3;下标N表示球粒陨石标准化值(Sun and McDonough, 1989);m/f= (FeOT/72)/(MgO/40);Gd是两批测试的结果,“\”代表没有测试数据.
      下载: 导出CSV
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