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    滇西“三江”地区临沧花岗岩基早-中奥陶世花岗质片麻岩的发现及其意义

    彭智敏 张辑 关俊雷 张璋 韩文文 付于真

    彭智敏, 张辑, 关俊雷, 张璋, 韩文文, 付于真, 2018. 滇西“三江”地区临沧花岗岩基早-中奥陶世花岗质片麻岩的发现及其意义. 地球科学, 43(8): 2571-2585. doi: 10.3799/dqkx.2018.102
    引用本文: 彭智敏, 张辑, 关俊雷, 张璋, 韩文文, 付于真, 2018. 滇西“三江”地区临沧花岗岩基早-中奥陶世花岗质片麻岩的发现及其意义. 地球科学, 43(8): 2571-2585. doi: 10.3799/dqkx.2018.102
    Peng Zhimin, Zhang Ji, Guan Junlei, Zhang Zhang, Han Wenwen, Fu Yuzhen, 2018. The Discovery of Early-Middle Ordovician Granitic Gneiss from the Giant Lincang Batholith in Sanjiang Area of Western Yunnan and Its Geological Implications. Earth Science, 43(8): 2571-2585. doi: 10.3799/dqkx.2018.102
    Citation: Peng Zhimin, Zhang Ji, Guan Junlei, Zhang Zhang, Han Wenwen, Fu Yuzhen, 2018. The Discovery of Early-Middle Ordovician Granitic Gneiss from the Giant Lincang Batholith in Sanjiang Area of Western Yunnan and Its Geological Implications. Earth Science, 43(8): 2571-2585. doi: 10.3799/dqkx.2018.102

    滇西“三江”地区临沧花岗岩基早-中奥陶世花岗质片麻岩的发现及其意义

    doi: 10.3799/dqkx.2018.102
    基金项目: 

    中国地质调查局项目 DD20160016

    国家自然科学基金项目 41273047

    国家自然科学基金项目 41303043

    详细信息
      作者简介:

      彭智敏(1978-), 男, 高级工程师, 主要从事区域地质调查工作

      通讯作者:

      张辑

    • 中图分类号: P597

    The Discovery of Early-Middle Ordovician Granitic Gneiss from the Giant Lincang Batholith in Sanjiang Area of Western Yunnan and Its Geological Implications

    • 摘要: 前人对"三江"地区临沧花岗岩基早古生代的岩浆事件研究极少.在双江地区临沧花岗岩基中首次识别出早古生代花岗质片麻岩.采用LA-ICP-MS锆石U-Pb定年、微区原位Hf同位素分析,结合全岩地球化学特征,对2件花岗质片麻岩样品进行了系统的研究.获得锆石U-Pb年龄分别为476.9±1.9 Ma、465.7±1.9 Ma,表明这些花岗质片麻岩形成于早-中奥陶世.花岗质片麻岩SiO2含量为70.67%~74.03%,K2O/Na2O值皆大于1,为1.04~1.55,属过铝质S型花岗岩.岩石微量元素特征显示其富集大离子亲石元素Rb、Th、U,亏损高场强元素Nb、Ta、Ti和Zr等,轻重稀土分异明显,轻稀土相对富集、重稀土亏损,具有明显的负Eu异常.2件样品锆石εHft)均为负值(-7.2~-0.7,均值-3.0),Hf同位素地壳模式年龄(tDMC)均值基本一致(1 639 Ma、1 630 Ma),说明花岗质片麻岩可能来源于古老地壳物质的部分熔融.综合分析表明,花岗质片麻岩是由原特提斯洋向东俯冲消减而引起的古老地壳物质部分熔融形成,是原特提斯俯冲消减的岩浆事件响应;说明在早奥陶世昌宁-孟连洋就存在俯冲消减,昌宁-孟连特提斯演化历史最早可以追溯到早奥陶世.

       

    • 图  1  云南双江县花岗质片麻岩地质简图

      图b据王保弟等(2013)修改.Ⅰ1-1.腾冲-盈江岩浆弧;Ⅰ2.潞西-三台山结合带;Ⅰ3.保山-镇康地块;Ⅱ1-1.昌宁-孟连结合带;Ⅱ2-1.临沧-勐海岩浆弧;Ⅲ1.南澜沧江结合带;Ⅴ.思茅地块;Ⅵ1-1.盈江岩浆弧;Ⅶ1.哀牢山结合带

      Fig.  1.  Geological sketch map for granitic gneiss from Shuangjiang area of western Yunnan

      图  2  野外露头照片(a、c)和显微照片(b、d)

      Fig.  2.  Outcrop photograph (a, c) and microstructural photomicrographs (b, d) for granitic gneiss

      图  3  花岗质片麻岩的锆石CL图像

      图a为样品D5279;图b为样品D3104.实线和虚线圆圈分别为U-Pb年龄和Hf同位素测点;括号外数值表示年龄,括号内数值表示锆石Hf同位素组成

      Fig.  3.  Zircon CL images for granitic gneiss

      图  4  花岗质片麻岩锆石U-Pb年龄谐和图

      Fig.  4.  Zircon U-Pb concordia diagrams of granitic gneiss

      图  5  花岗质片麻岩TAS图解(a)和K2O-SiO2图解(b)

      图a据Middlemost (1994);图b中实线据Peccerillo and Taylor (1976),虚线据Middlemost (1985)

      Fig.  5.  TAS diagram (a) and K2O-SiO2 diagram (b) for granitic gneiss

      图  6  花岗质片麻岩球粒陨石标准化REE配分模式(a)和原始地幔标准化微量元素蛛网图(b)

      标准化数值据Sun and McDonough(1989)

      Fig.  6.  Chondrite-normalized REE pattern (a) and primitive mantle-normalized trace element spider diagram (b) for granitic gneiss

      图  7  花岗质片麻岩C/MF-A/MF(a)和Rb/Sr-Rb/Ba(b)图解

      图a据Altherr et al.(2000);A.变质泥岩部分熔融;B.变质杂砂岩部分熔融;C.基性岩的部分熔融.图b据Sylvester(1998)

      Fig.  7.  C/MF-A/MF diagram (a) and Rb/Sr-Rb/Ba diagram (b) of granitic gneiss

      图  8  花岗质片麻岩锆石εHf(t)组成及εHf(t)-t图解

      Fig.  8.  εHf(t) composition and εHf(t)-t diagram for zircons for granitic gneiss

      表  1  花岗质片麻岩锆石U-Pb年龄分析结果

      Table  1.   Zircon U-Pb dating results for granitic gneiss

      测点号 元素含量(10-6) Th/U 同位素比值 年龄(Ma)
      Th U 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ
      D5279-01 81 106 0.76 0.062 8 0.002 6 1.136 0 0.047 3 0.130 7 0.002 0 702 88.9 771 22.5 792 11.2
      D5279-02 95 518 0.18 0.053 9 0.001 6 0.578 9 0.016 3 0.077 7 0.000 7 365 66.7 464 10.5 482 4.1
      D5279-03 117 408 0.29 0.056 6 0.001 6 0.605 1 0.017 1 0.077 2 0.000 9 476 93.5 480 10.8 480 5.4
      D5279-04 99 274 0.36 0.056 6 0.001 5 0.608 9 0.016 9 0.077 7 0.000 8 472 93.5 483 10.7 482 5.0
      D5279-05 88 516 0.17 0.054 7 0.001 4 0.586 0 0.015 4 0.077 3 0.000 9 467 57.4 468 9.9 480 5.1
      D5279-06 80 366 0.22 0.056 0 0.001 7 0.598 5 0.016 9 0.077 4 0.000 7 454 64.8 476 10.8 480 4.4
      D5279-07 162 444 0.36 0.066 7 0.001 7 1.117 4 0.038 1 0.120 1 0.002 7 828 52.9 762 18.3 731 15.6
      D5279-08 73 573 0.13 0.056 5 0.001 5 0.609 0 0.017 4 0.077 7 0.001 0 472 57.4 483 11.0 482 6.0
      D5279-09 83 561 0.15 0.055 6 0.001 6 0.598 3 0.019 0 0.077 9 0.001 4 435 66.7 476 12.1 484 8.6
      D5279-10 71 515 0.14 0.058 3 0.001 4 0.621 7 0.015 5 0.077 1 0.000 9 539 51.8 491 9.7 479 5.3
      D5279-11 95 780 0.12 0.064 2 0.001 3 0.976 7 0.021 0 0.109 7 0.001 0 750 44.4 692 10.8 671 5.9
      D5279-12 75 373 0.20 0.055 0 0.001 9 0.581 6 0.020 9 0.076 4 0.001 0 413 77.8 466 13.4 475 6.0
      D5279-13 75 443 0.17 0.056 1 0.001 6 0.596 4 0.016 7 0.077 0 0.000 7 457 63.0 475 10.6 478 4.3
      D5279-14 72 477 0.15 0.057 8 0.001 3 0.613 6 0.014 0 0.076 9 0.000 7 520 50.0 486 8.8 477 4.3
      D5279-15 144 905 0.16 0.056 2 0.001 2 0.600 3 0.013 6 0.077 2 0.000 7 461 46.3 477 8.6 479 4.4
      D5279-16 94 426 0.22 0.056 0 0.001 5 0.587 9 0.016 2 0.076 1 0.000 7 450 59.3 470 10.3 473 4.2
      D5279-17 86 377 0.23 0.054 3 0.001 9 0.573 8 0.021 3 0.076 6 0.000 8 389 81.5 460 13.8 476 4.7
      D5279-18 96 425 0.23 0.054 9 0.001 7 0.573 0 0.016 9 0.075 9 0.000 7 409 68.5 460 11.0 472 4.1
      D5279-19 78 427 0.18 0.055 7 0.001 4 0.588 1 0.015 7 0.076 5 0.000 8 439 52.8 470 10.1 475 4.6
      D5279-20 97 454 0.21 0.057 9 0.001 5 0.615 9 0.018 3 0.077 1 0.001 2 524 55.5 487 11.5 479 7.4
      D5279-21 98 411 0.24 0.057 6 0.001 5 0.616 3 0.021 0 0.076 8 0.001 4 522 59.3 487 13.2 477 8.7
      D5279-22 110 399 0.28 0.056 8 0.001 6 0.604 6 0.018 1 0.076 9 0.001 1 483 63.0 480 11.4 478 6.8
      D5279-23 68 413 0.16 0.058 9 0.001 8 0.619 8 0.018 7 0.076 0 0.000 7 565 68.5 490 11.7 472 4.3
      D5279-24 65 351 0.19 0.056 7 0.001 6 0.600 5 0.017 3 0.076 2 0.000 7 480 64.8 478 11.0 474 4.1
      D5279-25 63 407 0.15 0.057 5 0.001 8 0.608 8 0.018 7 0.076 2 0.000 7 509 66.7 483 11.8 473 4.0
      D5279-26 137 410 0.33 0.056 4 0.002 0 0.602 3 0.021 8 0.076 9 0.000 8 478 77.8 479 13.8 477 5.0
      D5279-27 69 417 0.17 0.056 0 0.001 5 0.592 8 0.015 4 0.076 3 0.000 6 450 59.3 473 9.8 474 3.8
      D5279-28 80 879 0.09 0.056 4 0.001 2 0.605 4 0.015 3 0.077 1 0.001 1 478 48.1 481 9.7 479 6.9
      D5279-29 142 471 0.30 0.066 6 0.001 5 1.311 2 0.029 8 0.141 5 0.001 0 833 48.1 851 13.1 853 5.5
      D3104-01 187 477 0.39 0.057 1 0.001 4 0.602 3 0.015 6 0.075 8 0.000 8 498 53.7 479 9.9 471 4.7
      D3104-02 222 1 280 0.17 0.056 8 0.001 3 0.591 7 0.012 8 0.074 9 0.000 6 483 48.1 472 8.2 466 3.7
      D3104-03 132 365 0.36 0.057 8 0.001 9 0.611 5 0.019 9 0.076 2 0.000 9 524 72.2 485 12.6 473 5.4
      D3104-04 87 218 0.40 0.067 5 0.002 0 1.357 4 0.038 6 0.145 4 0.001 4 854 65.7 871 16.6 875 8.1
      D3104-05 205 2 404 0.09 0.057 2 0.001 2 0.600 5 0.014 4 0.075 7 0.001 1 498 48.1 478 9.1 470 6.4
      D3104-06 65 209 0.31 0.056 2 0.002 0 0.578 2 0.020 8 0.074 9 0.001 0 461 81.5 463 13.4 466 5.7
      D3104-07 89 636 0.14 0.056 5 0.001 6 0.589 6 0.021 9 0.074 8 0.001 3 472 97.2 471 14.0 465 7.8
      D3104-08 217 412 0.53 0.057 2 0.001 6 0.592 6 0.017 9 0.074 7 0.000 9 502 64.8 473 11.4 464 5.1
      D3104-09 117 363 0.32 0.058 0 0.001 7 0.599 0 0.017 9 0.074 8 0.000 8 528 66.7 477 11.4 465 4.7
      D3104-10 357 996 0.36 0.056 7 0.001 5 0.590 4 0.015 5 0.075 3 0.001 0 480 83.3 471 9.9 468 5.9
      D3104-11 138 611 0.23 0.056 4 0.001 7 0.596 1 0.020 8 0.076 4 0.001 5 478 100.9 475 13.2 475 8.9
      D3104-12 258 307 0.84 0.056 0 0.001 6 0.582 4 0.017 2 0.075 2 0.000 6 450 67.6 466 11.0 467 3.7
      D3104-13 71 1 358 0.05 0.110 3 0.001 7 4.160 4 0.071 1 0.272 4 0.002 6 1806 27.6 1 666 14.0 1 553 13.1
      D3104-14 168 740 0.23 0.056 9 0.001 3 0.586 9 0.014 8 0.074 4 0.000 7 487 51.8 469 9.5 463 4.4
      D3104-15 277 1 458 0.19 0.055 8 0.001 1 0.576 2 0.012 1 0.074 6 0.000 7 455 10.2 462 7.8 464 3.9
      D3104-16 138 1 034 0.13 0.056 4 0.001 3 0.581 5 0.015 2 0.074 5 0.001 0 477 51.8 465 9.8 463 6.3
      D3104-17 116 265 0.44 0.059 9 0.002 2 0.621 0 0.025 2 0.074 8 0.001 2 598 79.6 490 15.8 465 7.3
      D3104-18 131 620 0.21 0.054 2 0.001 2 0.561 7 0.014 7 0.075 0 0.001 1 389 51.8 453 9.5 466 6.8
      D3104-19 63 252 0.25 0.055 9 0.001 8 0.578 1 0.018 7 0.074 7 0.000 7 455 70.4 463 12.0 465 4.2
      D3104-20 135 463 0.29 0.053 3 0.001 6 0.556 0 0.017 8 0.075 4 0.001 0 343 68.5 449 11.6 468 6.2
      D3104-21 211 1 565 0.13 0.055 0 0.001 2 0.573 1 0.013 0 0.075 3 0.001 0 413 48.1 460 8.4 468 5.7
      D3104-22 107 282 0.38 0.053 7 0.001 8 0.553 0 0.018 9 0.074 3 0.000 7 367 75.9 447 12.4 462 4.4
      D3104-23 204 1 352 0.15 0.055 6 0.001 2 0.576 6 0.013 2 0.074 8 0.000 9 435 46.3 462 8.5 465 5.2
      D3104-24 114 348 0.33 0.055 4 0.001 6 0.574 6 0.017 0 0.075 0 0.000 8 432 64.8 461 11.0 466 4.8
      D3104-25 146 289 0.51 0.059 1 0.001 8 0.616 1 0.019 0 0.075 1 0.000 7 572 64.8 487 12.0 467 4.4
      D3104-26 244 526 0.46 0.053 1 0.001 5 0.550 6 0.015 5 0.075 1 0.000 9 332 30.6 445 10.1 467 5.7
      D3104-27 122 375 0.33 0.056 1 0.001 6 0.582 9 0.017 9 0.075 0 0.001 0 454 63.0 466 11.5 466 5.8
      D3104-28 260 636 0.41 0.055 8 0.001 5 0.573 6 0.015 3 0.074 1 0.000 6 443 59.3 460 9.9 461 3.5
      D3104-29 168 341 0.49 0.055 3 0.001 7 0.568 8 0.017 3 0.074 9 0.001 4 433 70.4 457 11.2 465 8.2
      D3104-30 166 737 0.23 0.056 9 0.001 3 0.586 8 0.017 0 0.074 0 0.001 3 487 84.2 469 10.9 462 7.9
      下载: 导出CSV

      表  2  花岗质片麻岩锆石Hf同位素分析数据

      Table  2.   Zircon Lu-Hf isotope data for granitic gneiss

      测点号 t(Ma) 176Yb/177Hf 176Lu/177Hf 176Hf/177Hf 2σ εHf(0) εHf(t) tDM (Ma) tDMC(Ma) fLu/Hf
      D5279-1.1 480 0.079 585 0.002 970 0.282 453 0.000 010 -11.3 -1.7 1 192 1 554 -0.91
      D5279-2.1 480 0.027 221 0.001 026 0.282 375 0.000 008 -14.0 -3.8 1 239 1 690 -0.97
      D5279-3.1 482 0.063 853 0.002 427 0.282 399 0.000 010 -13.2 -3.3 1 252 1 662 -0.93
      D5279-4.1 484 0.067 342 0.002 585 0.282 441 0.000 010 -11.7 -1.9 1 196 1 571 -0.92
      D5279-5.1 473 0.062 514 0.002 321 0.282 477 0.000 010 -10.4 -0.7 1 135 1 491 -0.93
      D5279-6.1 472 0.072 551 0.002 664 0.282 417 0.000 009 -12.6 -3.0 1 234 1 633 -0.92
      D5279-7.1 475 0.066 997 0.002 466 0.282 428 0.000 012 -12.2 -2.5 1 211 1 602 -0.93
      D5279-8.1 474 0.038 219 0.001 495 0.282 287 0.000 009 -17.14 -7.2 1 379 1 907 -0.95
      D3104-1.1 471 0.058 272 0.002 182 0.282 453 0.000 011 -11.3 -1.6 1 166 1 543 -0.93
      D3104-2.1 470 0.072 773 0.002 835 0.282 404 0.000 011 -13.0 -3.6 1 259 1 666 -0.91
      D3104-3.1 465 0.068 827 0.002 759 0.282 387 0.000 010 -13.6 -4.2 1 281 1705 -0.92
      D3104-4.1 468 0.063 461 0.002 451 0.282 409 0.000 013 -12.8 -3.3 1 238 1 648 -0.93
      D3104-5.1 467 0.085 082 0.003 314 0.282 437 0.000 016 -11.9 -2.6 1 228 1 604 -0.90
      D3104-6.1 465 0.043 073 0.001 675 0.282 410 0.000 011 -12.8 -3.1 1 212 1 633 -0.95
      D3104-7.1 468 0.119 671 0.004 577 0.282 428 0.000 010 -12.2 -3.3 1 287 1 648 -0.86
      D3104-8.1 466 0.044 207 0.001 651 0.282 433 0.000 009 -12.0 -2.2 1 177 1 580 -0.95
      D3104-9.1 461 0.061 855 0.002 344 0.282 412 0.000 010 -12.7 -3.3 1 230 1 643 -0.93
      下载: 导出CSV

      表  3  花岗质片麻岩的主量元素(%)和微量元素(10-6)分析结果

      Table  3.   Major elements (%) and trace elements (10-6) analysis data for granitic gneiss

      样品号 D5279-H1 D5279-H2 D5279-H3 D3104-H1 D3104-H2 D3104-H3 D3104-H4
      SiO2 70.67 71.60 71.46 73.01 72.6 72.37 74.03
      TiO2 0.46 0.45 0.44 0.28 0.30 0.29 0.26
      Al2O3 14.27 14.51 14.10 13.24 14.00 13.89 13.64
      Fe2O3T 3.66 3.50 3.50 2.68 2.80 2.77 2.21
      MnO 0.06 0.05 0.05 0.06 0.10 0.07 0.05
      MgO 0.75 0.74 0.71 0.57 0.60 0.59 0.46
      CaO 2.20 2.24 2.18 1.58 2.00 1.77 1.39
      Na2O 2.97 3.13 3.08 2.73 3.30 3.08 2.75
      K2O 3.67 3.52 3.52 4.22 3.50 3.99 4.11
      P2O5 0.12 0.11 0.11 0.06 0.10 0.07 0.06
      LOI 0.51 0.70 0.58 0.85 0.60 0.59 0.85
      Total 99.33 100.54 99.74 99.29 99.9 99.47 99.79
      A/CNK 1.11 1.11 1.10 1.11 1.09 1.10 1.19
      Sc 10.6 10.1 9.72 9.30 9.69 9.03 8.56
      V 42.6 41.8 40.9 28.7 29.7 30.0 26.2
      Cr 10.4 9.39 9.28 5.10 5.23 4.89 4.27
      Co 5.71 5.71 5.29 3.73 4.39 3.84 2.33
      Ni 4.98 4.46 4.86 2.57 2.82 2.80 2.02
      Ga 19.1 19.3 18.5 15.4 16.7 16.2 15.7
      Rb 165 156 158 183 153 170 161
      Sr 79.8 81.2 78.3 60.3 72.9 68.4 60.0
      Y 51.5 48.3 54.2 54.4 50.3 59.3 54.9
      Zr 216 240 241 128 121 118 121
      Nb 12.4 12.2 11.9 9.37 10.3 9.66 8.69
      Cs 7.71 6.23 7.40 5.66 6.69 5.47 3.25
      Ba 726 748 693 450 398 504 436
      La 45.2 46.0 36.7 26.9 27.8 29.9 30.1
      Ce 93.1 94.3 76.1 56.2 58.5 62.9 64.2
      Pr 10.3 10.9 8.63 6.43 6.67 7.23 7.19
      Nd 40.3 41.8 33.5 24.5 25.5 27.5 27.8
      Sm 8.62 9.04 7.36 5.78 6.11 6.30 6.58
      Eu 1.09 1.15 1.08 0.69 0.73 0.76 0.66
      Gd 8.54 8.78 7.58 6.61 6.68 7.26 7.01
      Tb 1.45 1.36 1.37 1.20 1.29 1.36 1.32
      Dy 8.60 8.07 8.52 8.21 8.31 9.11 8.54
      Ho 1.69 1.62 1.75 1.77 1.65 1.91 1.81
      Er 5.00 4.66 5.12 5.46 4.69 5.65 5.48
      Tm 0.69 0.65 0.72 0.83 0.66 0.86 0.82
      Yb 4.57 4.46 4.86 5.68 4.22 5.54 5.34
      Lu 0.67 0.66 0.72 0.84 0.60 0.84 0.82
      Hf 6.54 7.30 7.10 4.35 4.04 3.92 4.07
      Ta 0.96 1.00 0.91 0.99 0.98 1.06 0.88
      Pb 26.4 27.4 26.0 34.5 29.1 31.1 30.7
      Th 24.5 26.4 19.4 16.6 16.5 18.6 20.5
      U 3.43 3.51 3.52 5.19 4.20 3.38 4.40
      δEu 0.34 0.35 0.34 0.30 0.39 0.40 0.44
      (La/Yb)N 3.40 4.73 3.87 4.04 7.08 7.39 5.41
      下载: 导出CSV
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    出版历程
    • 收稿日期:  2018-05-08
    • 刊出日期:  2018-08-15

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