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    南黄海千里岩岛榴辉岩变质演化P-T-t轨迹及其构造意义

    李敏 韩宗珠 许红 赵广涛 张贺 来志庆

    李敏, 韩宗珠, 许红, 赵广涛, 张贺, 来志庆, 2014. 南黄海千里岩岛榴辉岩变质演化P-T-t轨迹及其构造意义. 地球科学, 39(9): 1289-1300. doi: 10.3799/dqkx.2014.110
    引用本文: 李敏, 韩宗珠, 许红, 赵广涛, 张贺, 来志庆, 2014. 南黄海千里岩岛榴辉岩变质演化P-T-t轨迹及其构造意义. 地球科学, 39(9): 1289-1300. doi: 10.3799/dqkx.2014.110
    Li Min, Han Zongzhu, Xu Hong, Zhao Guangtao, Zhang He, Lai Zhiqing, 2014. Metamorphic P-T-t Path of Eclogites from Qianliyan Island in the South Yellow Sea and Its Tectonic Implications. Earth Science, 39(9): 1289-1300. doi: 10.3799/dqkx.2014.110
    Citation: Li Min, Han Zongzhu, Xu Hong, Zhao Guangtao, Zhang He, Lai Zhiqing, 2014. Metamorphic P-T-t Path of Eclogites from Qianliyan Island in the South Yellow Sea and Its Tectonic Implications. Earth Science, 39(9): 1289-1300. doi: 10.3799/dqkx.2014.110

    南黄海千里岩岛榴辉岩变质演化P-T-t轨迹及其构造意义

    doi: 10.3799/dqkx.2014.110
    基金项目: 

    国家专项 GZH201200510-02

    国家重点基础研究发展计划"973"项目 2012CB956004

    详细信息
      作者简介:

      李敏(1988-), 女, 博士研究生, 主要从事海洋地球化学与大陆边缘动力学研究.E-mail: liminjining@163.com

      通讯作者:

      韩宗珠, E-mail: hanzongzhu@ouc.edu.cn

    • 中图分类号: P595

    Metamorphic P-T-t Path of Eclogites from Qianliyan Island in the South Yellow Sea and Its Tectonic Implications

    • 摘要: 南黄海千里岩岛榴辉岩对进一步深入完善大别-苏鲁造山带的研究具有重要意义.岩相学和矿物学研究显示榴辉岩主要经历了俯冲进变质(Ⅰ)、峰期榴辉岩相变质(Ⅱ)、角闪岩相退变质(Ⅲ)和绿片岩相退变质(Ⅳ)阶段.各阶段的温压条件分别为: Ⅱ阶段T=806.3 ℃, P=3.32 GPa; Ⅲ阶段T=658.68 ℃, P=0.78 GPa; Ⅳ阶段T<550 ℃, P<0.3 GPa.锆石SHRIMP U-Pb测年指示千里岩榴辉岩的原岩形成于新元古代(约747±19 Ma), 超高压变质作用发生在早三叠世(约241.1±1.5 Ma), 角闪岩相退变质发生在三叠纪末(约205.8 Ma).在此基础上, 建立了千里岩岛榴辉岩的P-T-t演化轨迹, 反映出榴辉岩经历了2个折返阶段.这一P-T-t轨迹整体上与苏鲁地区榴辉岩类似, 指示该区所在的千里岩隆起区是苏鲁造山带在海区的延伸.

       

    • 图  1  南黄海千里岩岛地质略图(据韩宗珠等, 2007; Li et al., 2011廖晶等, 2013)

      ①郯庐断裂;②青岛-烟台断裂;③青岛-荣成断裂;④五莲-青岛断裂;⑤千里岩断裂;⑥泗阳-连云港断裂;⑦千里岩隆起南缘断裂;⑧嘉山-响水断裂;⑨黄海东缘断裂;⑩青岛-荣成断裂、千里岩断裂、千里岩南缘断裂东延推测

      Fig.  1.  Geological sketch map of Qianliyan island in the South Yellow Sea

      图  2  榴辉岩矿物共生组合

      a、b.正交偏光;c.单偏光;d、e、f、g.BSE

      Fig.  2.  Mineral assemblage for eclogites

      图  3  千里岩岛榴辉岩主要矿物BSE、成分剖面图和成分分类

      a、b、c.石榴石;d、e、f.绿辉石;g、h、i.多硅白云母.图a、d、g中的实线为矿物成分剖面线

      Fig.  3.  BSE maps of main minerals of eclogites from Qianliyan island and the composition profile and triangle diagrams

      图  4  角闪石分类(Leake et al., 1997)

      Fig.  4.  Amphibole composition classification

      图  5  榴辉岩部分锆石高清阴极发光图像、测点位置和测年结果

      Fig.  5.  Cathode luminescence photo micrographs, measure points and dating results of zircons

      图  6  榴辉岩单颗粒锆石SHRIMP U-Pb年龄谐和图

      Fig.  6.  Single zircon SHRIMP U-Pb Concordia diagram for eclogites

      图  7  千里岩榴辉岩(a)及苏鲁地区(b)变质演化P-T-t轨迹

      Fig.  7.  P-T-t path of eclogites from Qianliyan and Sulu orogenic belt

      表  1  千里岩榴辉岩各变质阶段代表性矿物化学成分(%)

      Table  1.   The representative mineral compositions for eclogites from Qianliyan

      变质阶段 Ⅰ阶段 Ⅱ阶段 Ⅲ阶段 Ⅵ阶段
      Grt Omp Ep Grt Omp Phe Amp Ab Di Ep Chl Bt
      SiO2 38.746 55.460 38.150 39.010 56.540 56.810 43.280 67.920 52.980 37.710 26.210 36.940
      TiO2 0.024 0.050 22.960 0.020 0.010 0.270 0.120 0.010 0.050 22.340 0.060 0.140
      Al2O3 20.556 9.080 12.560 20.980 10.690 24.830 13.100 20.120 2.610 12.630 18.930 18.600
      FeO 25.89 6.85 - 24.14 5.39 0.03 17.15 0.48 9.56 - 30.68 18.62
      Cr2O3 0.042 0.030 - 0.040 0.030 3.160 0.040 - 0.040 - 0.030 0.070
      MnO 0.42 0.04 - 0.48 0.02 0.01 0.10 0.01 0.11 - 0.25 0.15
      MgO 3.889 8.210 0 5.230 7.490 4.160 10.090 0.110 11.690 0.080 13.930 11.550
      CaO 10.048 13.780 24.550 10.230 12.430 0 11.730 1.530 21.840 24.250 0.060 0
      Na2O 0.023 6.560 - 0.020 7.200 0.060 2.600 9.830 1.570 - 0.030 0.060
      K2O 0.012 0.020 - - 0.010 7.980 0.460 0.050 0.020 - 0.040 8.310
      总量 99.65 100.08 98.22 100.14 99.81 97.34 98.68 100.06 100.47 97.02 90.22 94.44
      O 12 6 25 12 6 11 23 8 6 25 14 22
      Si 3.05 1.99 6.00 3.02 2.02 3.63 6.37 2.97 1.96 6.01 2.76 5.59
      Al 1.906 0.380 4.250 1.920 0.450 1.870 2.270 1.040 0.110 4.190 2.35 -
      Fe3+ 0 0.09 1.65 0.05 0.02 - 0.43 - 0.07 1.68 - -
      Ti 0.001 0 - 0 0 0.010 0.010 0 0 - 0.010 0.020
      Fe2+ 1.705 0.120 - 1.520 0.140 0.170 1.690 0.020 0.220 - 2.710 2.360
      Cr 0.003 0 - 0 0 0 0 - 0 - 0 0.01
      Mn 0.028 0 - 0.03 0 0 0.01 0 0 - 0.02 0.02
      Mg 0.456 0.44 0 0.60 0.40 0.40 2.21 0.01 0.64 0.02 2.19 2.61
      Ca 0.848 0.530 4.140 0.850 0.480 0 1.850 0.070 0.870 4.140 0.010 0
      Na 0.004 0.450 - 0 0.500 0.010 0.740 0.830 0.110 - 0.010 0.020
      K 3.040 0 - - 0 0.650 0.090 0 0 - 0 1.61
      离子数 8 4 16 8 4 6.74 15.68 4.93 4 16.04 10.06 15.54
      下载: 导出CSV

      表  2  榴辉岩单颗粒锆石SHRIMP U-P定年结果

      Table  2.   SHRIMP U-Pb dating of single zircons of eclogites

      点号 U(10-6) Th(10-6) 232Th/238U 206Pb(10-6) 238Pb/206Pb 误差(%) 207Pb/206Pb 误差(%) 207Pb/235Pb 误差(%) 206Pb/238U Age(Ma) 误差(%)
      QLY-1-1.1 210 11 0.05 6.7 26.87 1.4 0.058 3 2.7 0.28 3.4 234.6 3.3
      QLY-1-2.1 312 217 0.72 19.7 13.60 1.1 0.063 5 1.4 0.61 2.7 455.5 5.0
      QLY-1-3.1 479 375 0.81 52.0 7.92 1.1 0.066 3 0.9 1.15 1.4 766.5 7.9
      QLY-1-3.2 436 19 0.04 14.7 25.42 1.2 0.071 7 2.6 0.27 8.0 242.8 3.1
      QLY-1-4.1 148 148 1.03 15.8 8.05 1.3 0.068 4 1.6 1.11 2.9 751.9 9.0
      QLY-1-4.2 812 976 1.24 83.2 8.38 1.1 0.064 1 0.7 1.05 1.3 726.8 7.3
      QLY-1-5.1 306 5 0.02 10.2 25.89 1.2 0.059 1 2.5 0.29 3.8 243.2 2.8
      QLY-1-6.1 350 12 0.04 11.3 26.65 1.2 0.057 1 2.0 0.26 4.9 235.5 2.8
      QLY-1-7.1 513 11 0.02 17.6 25.10 1.6 0.055 6 1.7 0.29 3.5 250.8 4.0
      QLY-1-8.1 597 49 0.08 19.6 26.18 1.1 0.055 5 1.5 0.29 2.2 241.3 2.7
      QLY-1-9.1 349 413 1.22 38.0 7.89 1.1 0.066 6 1.0 1.15 1.6 768.3 8.2
      QLY-1-10.1 327 17 0.05 10.6 26.54 1.2 0.057 6 3.0 0.28 4.7 237.2 2.8
      QLY-1-11.1 431 17 0.04 14.3 25.94 1.3 0.057 5 2.5 0.27 4.7 242.0 3.1
      QLY-1-12.1 215 6 0.03 7.2 25.56 1.2 0.059 8 5.2 0.28 8.1 245.4 3.1
      QLY-1-13.1 320 404 1.30 33.3 8.26 1.1 0.063 8 1.1 1.04 1.8 736.0 7.7
      QLY-1-14.1 278 4 0.02 9.2 25.98 1.2 0.057 2 3.8 0.27 5.9 241.8 2.9
      QLY-1-15.1 192 115 0.62 11.6 14.17 1.2 0.066 0 1.8 0.58 4.4 436.4 5.3
      QLY-1-16.1 242 4 0.02 8.1 25.64 1.8 0.059 8 3.8 0.27 7.2 244.2 4.5
      QLY-1-17.1 305 88 0.30 11.7 22.45 1.2 0.060 1 2.0 0.35 3.2 280.0 3.3
      QLY-1-18.1 276 20 0.07 10.1 23.44 1.2 0.058 2 2.1 0.32 3.6 268.4 3.1
      QLY-1-19.1 218 1 213 2 1.01 125.3 14.95 1.0 0.061 0 0.6 0.55 1.6 416.7 4.2
      QLY-1-20.1 343 19 0.06 11.2 26.42 1.3 0.056 3 2.3 0.27 4.0 238.5 3.0
      QLY-1-21.1 347 23 0.07 11.2 26.58 1.2 0.059 2 3.2 0.28 4.9 236.7 2.8
      QLY-1-22.1 254 13 0.05 7.1 30.52 1.2 0.055 3 2.4 0.21 6.5 205.8 2.5
      QLY-1-23.1 430 27 0.06 14.3 25.86 1.1 0.055 2 2.1 0.26 2.8 242.7 2.7
      QLY-1-24.1 487 26 0.05 16.4 25.54 1.1 0.056 0 1.7 0.27 4.1 245.8 2.8
      QLY-1-25.1 267 5 0.02 8.8 26.20 1.2 0.055 0 2.2 0.27 4.2 240.3 2.8
      QLY-1-26.1 196 79 0.41 15.2 11.05 1.3 0.067 9 1.8 0.81 2.8 556.7 7.1
      QLY-1-27.1 295 4 0.01 9.6 26.37 1.3 0.059 2 3.0 0.27 5.3 238.1 3.0
      QLY-1-28.1 255 7 0.03 8.3 26.31 1.6 0.057 2 3.1 0.26 6.1 238.6 3.8
      QLY-1-29.1 384 535 1.44 40.1 8.24 1.1 0.067 1 1.0 1.07 1.9 736.2 7.8
      QLY-1-30.1 340 453 1.38 33.4 8.77 1.5 0.065 0 1.1 0.98 2.2 694.4 10.2
      注: 锆石SHRIMP U-Pb测试在北京离子探针中心完成.
      下载: 导出CSV

      表  3  苏鲁超高压变质带榴辉岩中锆石SHRIMP U-Pb定年结果

      Table  3.   SHRIMP U-Pb dating for zircons from UHP metamorphic rocks in Sulu terrane

      样品号 地点 围岩类型 岩浆锆石年龄(Ma) 超高压变质年龄(Ma) 角闪岩相退变质年龄(Ma) 参考文献
      H2 三清阁 大理岩 - 231~238 234±4 210~220 214±4 Liu et al., 2007
      CT1 池塘 正片麻岩 650~795 226~236 231±3 -
      ZC 诸城 正片麻岩 710~812 223~229 227±2 -
      LSD-1 岚山头 正片麻岩 682~810 227~238 233±4 205~217 209±3 刘福来和薛怀民, 2007
      YK01 仰口 正片麻岩 652~796 222~230 226±3 201~214 207±2
      B42 钻孔MH 正片麻岩 682~820 224~238 232±3 211~217 214±5
      QLY-1 千里岩岛 副片麻岩 416~770 241.1±1.5 205.8 本文
      下载: 导出CSV
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