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    华北克拉通中部带云中山石榴斜长角闪岩变质演化及其构造意义

    郭敏洁 钱加慧 尹常青 张健 卢成森

    郭敏洁, 钱加慧, 尹常青, 张健, 卢成森, 2021. 华北克拉通中部带云中山石榴斜长角闪岩变质演化及其构造意义. 地球科学, 46(11): 3892-3909. doi: 10.3799/dqkx.2021.016
    引用本文: 郭敏洁, 钱加慧, 尹常青, 张健, 卢成森, 2021. 华北克拉通中部带云中山石榴斜长角闪岩变质演化及其构造意义. 地球科学, 46(11): 3892-3909. doi: 10.3799/dqkx.2021.016
    Guo Minjie, Qian Jiahui, Yin Changqing, Zhang Jian, Lu Chengsen, 2021. Metamorphic Evolution and Tectonic Implications of Garnet Amphibolite from Yunzhongshan Terrane in Central North China Craton. Earth Science, 46(11): 3892-3909. doi: 10.3799/dqkx.2021.016
    Citation: Guo Minjie, Qian Jiahui, Yin Changqing, Zhang Jian, Lu Chengsen, 2021. Metamorphic Evolution and Tectonic Implications of Garnet Amphibolite from Yunzhongshan Terrane in Central North China Craton. Earth Science, 46(11): 3892-3909. doi: 10.3799/dqkx.2021.016

    华北克拉通中部带云中山石榴斜长角闪岩变质演化及其构造意义

    doi: 10.3799/dqkx.2021.016
    基金项目: 

    国家自然科学基金项目 41972197

    国家自然科学基金项目 41890831

    广东省基础与应用基础研究基金项目 2019A1515012189

    中央高校基本科研业务费 18lgpy17

    详细信息
      作者简介:

      郭敏洁(1996-), 女, 硕士生, 主要从事变质地质学研究.ORCID: 0000-0002-4539-5523.E-mail: guomj5@mail2.sysu.edu.cn

      通讯作者:

      钱加慧, ORCID: 0000-0003-1119-8035.E-mail: qianjh5@mail.sysu.edu.cn

    • 中图分类号: P588

    Metamorphic Evolution and Tectonic Implications of Garnet Amphibolite from Yunzhongshan Terrane in Central North China Craton

    • 摘要: 云中山地体位于华北克拉通中部造山带中部,是衔接吕梁地体和五台-恒山地体的关键位置.确定云中山地体的变质作用演化历史可为深入理解吕梁-云中山-五台-恒山地区的整体地质过程提供重要限定.对云中山石榴斜长角闪岩开展了详细的岩石学、相平衡模拟和锆石年代学研究.两个代表性样品均具有顺时针变质P-T-t轨迹,峰期阶段位于金红石稳定域,温压条件分别为0.96±0.11 GPa/720±8.0℃(L1903)和1.26±0.08 GPa/756±14.0℃(L1906);峰期后发生降压作用,金红石转变成钛铁矿,石榴石边部生长斜长石(+普通角闪石)冠状边,普通角闪石转变成镁铁闪石;晚期阶段以冷却为主,石榴石的边部出现少量绿泥石交代.对两个样品的岩石组构和化学成分对比表明,石榴斜长角闪岩的部分熔融受全岩成分影响,岩石贫硅钠而富铁镁钛时难熔,反之则易熔.样品变质锆石的U-Pb定年结果为1 928~1 806 Ma.这些锆石相对富集重稀土,利用锆石Ti温度计计算的结晶温度为520~680℃,与岩石的冷却温度相近,因此所获年龄应代表退变冷却时代.吕梁-云中山-五台-恒山地区的整体地质特征对比表明,云中山地体的岩石-地层组成和变质作用演化与五台-恒山地体非常相似,记录了古元古代晚期的碰撞造山事件.

       

    • 图  1  华北克拉通中部造山带构造简图(a)和吕梁‒云中山地区地质图(b)

      a.据Zhao et al.(2007);b.据Zhao et al.(2008)王惠初等(2020)修改. 图a中变质杂岩体缩写:HS.恒山;WF.五台;FP.阜平

      Fig.  1.  Simplified tectonic map of the Trans-North China Orogen (a) and geological map of the Lüliang-Yunzhongshan area (b)

      图  2  云中山地体石榴斜长角闪岩样品的野外照片

      Fig.  2.  Field photographs of garnet amphibolite samples in the Yunzhongshan terrane

      图  3  云中山地体石榴斜长角闪岩样品的岩相学照片

      a.(L1903)石榴石变斑晶包裹普通角闪石、金红石、钛铁矿和石英,“包裹体”型斜长石生长于裂隙,长红线表示石榴石成分环带的位置;b.(L1903)石榴石变斑晶包裹普通角闪石、钛铁矿和石英,“包裹体”型斜长石生长于裂隙;石榴石边部可见绿泥石交代,普通角闪石可见镁铁闪石边;c.(L1903)基质矿物主要为普通角闪石、斜长石、钛铁矿、镁铁闪石和石英;d.(L1906)石榴石变斑晶被斜长石(+普通角闪石)冠状边结构包围.斜长石的An值从冠状边向基质逐渐降低;e.(L1906)石榴石含有钛铁矿和石英包裹体;f.(L1906)基质矿物组成主要为普通角闪石、斜长石、钛铁矿和石英

      Fig.  3.  Photomicrographs of garnet amphibolite samples from the Yunzhongshan terrane

      图  4  云中山地体石榴斜长角闪岩样品的石榴石成分分带

      镁铝榴石(Xpy=Mg/(Fe2++Mg+Ca+Mn);XgrXspsXalm定义方式相同)、钙铝榴石Xgr、锰铝榴石Xsps和铁铝榴石Xalm.R1、C和R2分别与表 2图 3a图 3d对应

      Fig.  4.  Compositional zoning of garnet in the garnet amphibolite samples from the Yunzhongshan terrane

      图  5  云中山地体石榴斜长角闪岩样品的斜长石An值图解(a)和角闪石成分分类图(b)

      Fig.  5.  A diagram showing the An value of plagioclase compositions (a) and a classification diagram showing compositions of hornblende (b) in garnet amphibolite samples from the Yunzhongshan terrane

      图  6  云中山地体石榴斜长角闪岩样品的P-TT-XH2O视剖面图

      a. NCFMASHTO体系下L1903样品的P-T视剖面图,石英和水设为过量;b. L1903样品主要矿物的成分等值线,石榴石的镁铝榴石py(=Mg/(Fe2++Mg+Ca))、钙铝榴石gr(=Ca/(Fe2++Mg+Ca)),斜长石An(=Ca/(Ca+Na)),普通角闪石Ti和M2位Al;c. NCKFMASHTO体系下L1906的T-XH2O视剖面图,压力为0.95 GPa,石英设为过量.垂直虚线表示图 6d中的水含量;d. L1906样品的P-T视剖面图,矿物成分等值线包括斜长石An(=Ca/(Ca+Na+K))、石榴石的镁铝榴石py(=Mg/(Fe2++Mg+Ca))、普通角闪石Ti和M2位Al.全岩成分通过XRF测试得到,摩尔百分比归一化后结果见表 1

      Fig.  6.  The P-T and T-XH2O pseudosection of garnet amphibolite samples from the Yunzhongshan terrane

      图  7  云中山地体石榴斜长角闪岩样品的锆石阴极发光图像及U-Pb年龄谐和图

      a,c. 样品L1903和L1906的锆石阴极发光图像,红圈表示LA-ICP-MS分析点位,标注的编号、207Pb/206Pb年龄(Ma)及Th/U比值分别与表 3对应;b. L1903样品的年龄谐和图,蓝圈旁注明207Pb/206Pb年龄和Th/U比值;d. L1906样品的年龄谐和图,蓝圈为Ⅰ型锆石测点结果,且计算得到加权平均年龄;灰圈表示Ⅱ型锆石测点结果,Pb丢失明显

      Fig.  7.  Cathodoluminescence images of zircon and concordia diagrams of U-Pb dating results of garnet amphibolite samples from the Yunzhongshan terrane

      图  8  云中山地体石榴斜长角闪岩样品锆石的球粒陨石标准化稀土元素模式

      球粒陨石的数据引自Sun and McDonough(1989)

      Fig.  8.  Chondrite-normalized REE patterns of zircon of garnet amphibolite samples from the Yunzhongshan terrane

      图  9  吕梁‒云中山‒五台‒恒山地区代表性变质P-T轨迹

      1.五台石榴斜长角闪岩(Qian and Wei, 2016);2.南恒山石榴斜长角闪岩(Qian and Wei, 2016);3.北恒山高压麻粒岩(Zhang et al., 2013);4.吕梁变泥质岩(于津海等,2004);5.吕梁石榴斜长角闪岩(Zhao et al., 2010);6.吕梁基性麻粒岩(Xiao et al., 2017);7.吕梁泥质片麻岩(Zhao et al., 2017);8.云中山石榴斜长角闪岩L1903(本文);9.云中山石榴斜长角闪岩L1906(本文).虚线ru(L1903)表示L1903样品金红石的出现线.变质相的划分引自Wei and Duan(2018)

      Fig.  9.  The representative P-T paths for metamorphic rocks from the Lüliang-Yunzhongshan-Wutai-Hengshan areas

      图  10  吕梁‒云中山‒五台‒恒山地区代表性变质年龄的直方图

      年龄资料引自Kröner et al.(2006)Zhao et al.(2008)Qian et al.(2013, 2015, 2017, 2019, 2021);Zhang et al.(2013, 2018);Qian and Wei(2016)Xiao et al.(2017, 2019);Zhao et al.(2017)米广尧等(2018)Liu et al.(2020)和本文数据

      Fig.  10.  Histogram of representative metamorphic ages from the Lüliang-Yunzhongshan-Wutai-Hengshan areas

      表  1  云中山地体石榴斜长角闪岩样品的全岩成分及标准化摩尔比

      Table  1.   Bulk-rock compositions and their normalized mole-proportions of garnet amphibolite samples from the Yunzhongshan terrane

      质量百分比(wt.%) SiO2 TiO2 Al2O3 Fe2O3T MnO MgO CaO Na2O K2O P2O5 LOI XMg
      L1903 48.31 2.27 14.06 17.41 0.23 5.89 9.61 0.81 0.40 0.38 0.30 0.40
      L1906-01 60.60 0.68 17.24 7.32 0.12 2.32 5.81 4.43 0.60 0.13 0.52 0.39
      L1906-02 61.96 0.67 16.98 6.60 0.10 2.09 6.13 4.22 0.40 0.12 0.35 0.39
      摩尔比(%) H2O SiO2 Al2O3 CaO MgO FeO K2O Na2O TiO2 O XMg
      L1903 52.80 9.06 10.66 9.59 14.32 0.85 1.86 0.85 0.40 图 7a7b
      L1906-02 0.00 67.58 10.91 6.98 3.40 5.41 0.28 4.46 0.55 0.43 0.39 图 7c
      L1906-02 5.00 64.20 10.37 6.63 3.23 5.14 0.26 4.24 0.52 0.40 0.39 图 7c
      L1906-02 1.68 66.45 10.73 6.86 3.34 5.32 0.27 4.38 0.54 0.42 0.39 图 7d
      注:XMg=Mg/(Mg+Fe) (mol%);Fe2O3T代表全铁;L1906-01和L1906-02表示采自同一块岩石样品,进行主量成分平行对比测试,其中L1906-02用于下文相平衡模拟.
      下载: 导出CSV

      表  2  云中山地体石榴斜长角闪岩L1903和L1906样品的电子探针分析结果

      Table  2.   Microprobe analyses for garnet amphibolite samples L1903 and L1906 from the Yunzhongshan terrane

      样品 L1903 L1906
      矿物 g-C g-R1 g-R2 pl-包体 pl-基质 hb-包体 hb-基质1 hb-基质2 chl cumm ilm g-C g-R1 g-R2 hb-冠状边 hb-基质1 hb-基质2 pl-冠状边 pl-基质 chl ilm
      SiO2 36.71 37.87 36.89 45.56 43.85 43.24 42.51 42.59 27.95 52.40 0.04 34.97 35.72 36.61 41.20 41.20 42.34 54.80 58.41 21.95 0.01
      TiO2 0.11 0.00 0.06 0.02 0.67 0.84 0.70 0.83 1.35 0.05 54.04 0.04 0.02 0.00 0.73 0.64 0.49 0.02 0.02 0.02 51.06
      Al2O3 20.83 20.74 20.38 34.70 12.02 13.23 12.54 14.10 16.48 0.70 0.01 20.54 20.50 20.52 13.40 13.07 13.26 23.83 23.71 19.78 0.00
      Cr2O3 0.08 0.06 0.01 0.03 0.03 0.07 0.04 0.06 0.05 0.00 0.07 0.02 0.00 0.05 0.05 0.00 0.02 0.00 0.02 0.03 0.02
      Fe2O3 2.79 1.01 1.58 0.14 21.48 0.88 3.57 2.28 0.00 0.08 0.00 3.00 1.82 0.87 5.28 4.56 2.88 0.71 0.00 0.00 1.52
      FeO 25.83 29.10 29.53 0.00 0.00 15.33 14.65 15.85 27.02 29.70 46.63 29.51 30.25 32.05 14.67 14.43 14.97 0.00 0.00 37.80 45.31
      MnO 1.61 1.39 2.10 0.00 0.07 0.11 0.09 0.14 0.04 0.49 0.59 1.24 1.65 2.01 0.12 0.22 0.19 0.06 0.00 0.65 0.53
      MgO 2.38 2.33 1.87 0.00 8.37 8.74 8.47 7.98 12.06 13.23 0.25 3.39 2.67 2.10 7.75 8.11 8.10 0.04 0.00 4.00 0.02
      CaO 9.50 8.18 7.09 19.29 11.46 11.80 11.24 11.49 0.44 0.80 0.07 3.86 4.61 4.53 10.79 11.06 11.08 9.39 5.60 0.07 0.00
      Na2O 0.02 0.03 0.02 1.02 0.87 1.00 0.87 1.04 0.10 0.01 0.03 0.02 0.03 0.03 1.14 1.21 1.01 7.10 8.24 0.06 0.01
      K2O 0.01 0.00 0.00 0.00 0.34 0.43 0.36 0.44 0.57 0.01 0.00 0.00 0.00 0.00 0.32 0.35 0.26 0.05 0.17 0.00 0.00
      Totals 99.87 100.71 99.53 100.76 99.16 95.67 95.04 96.80 86.06 97.47 101.73 96.59 97.27 98.77 95.45 94.85 94.60 96.00 96.17 84.36 98.48
      Oxygens 12.00 12.00 12.00 8.00 8.00 23.00 23.00 23.00 14.00 23.00 3.00 12.00 12.00 12.00 23.00 23.00 23.00 8.00 8.00 14.00 3.00
      Si 2.93 3.00 2.98 2.09 2.19 6.54 6.50 6.41 3.04 7.93 0.00 2.90 2.95 2.99 6.32 6.35 6.50 2.58 2.70 2.62 0.00
      Ti 0.01 0.00 0.00 0.00 0.03 0.10 0.08 0.09 0.11 0.01 1.00 0.00 0.00 0.00 0.08 0.07 0.06 0.00 0.00 0.00 0.99
      Al 1.96 1.94 1.94 1.88 0.71 2.36 2.26 2.50 2.11 0.13 0.00 2.01 1.99 1.98 2.42 2.38 2.40 1.33 1.29 2.79 0.00
      Cr 0.01 0.00 0.00 0.00 0.00 0.01 0.01 0.01 0.00 0.00 0.00 0.00 0.00 0.00 0.01 0.00 0.00 0.00 0.00 0.00 0.00
      Fe3+ 0.17 0.06 0.10 0.01 0.81 0.10 0.41 0.26 0.00 0.01 0.00 0.19 0.11 0.05 0.61 0.53 0.33 0.03 0.00 0.00 0.03
      Fe2+ 1.72 1.93 1.99 0.00 0.00 1.94 1.87 1.99 2.46 3.76 0.96 2.05 2.09 2.19 1.88 1.86 1.92 0.00 0.00 3.78 0.97
      Mn 0.11 0.09 0.14 0.00 0.00 0.01 0.01 0.02 0.00 0.06 0.01 0.09 0.12 0.14 0.02 0.03 0.03 0.00 0.00 0.07 0.01
      Mg 0.28 0.28 0.23 0.00 0.62 1.97 1.93 1.79 1.96 2.98 0.01 0.42 0.33 0.26 1.77 1.86 1.85 0.00 0.00 0.71 0.00
      Ca 0.81 0.70 0.61 0.95 0.61 1.91 1.84 1.85 0.05 0.13 0.00 0.34 0.41 0.40 1.77 1.83 1.82 0.47 0.28 0.01 0.00
      Na 0.00 0.01 0.00 0.09 0.08 0.29 0.26 0.30 0.02 0.00 0.00 0.00 0.01 0.01 0.34 0.36 0.30 0.65 0.74 0.01 0.00
      K 0.00 0.00 0.00 0.00 0.02 0.08 0.07 0.08 0.08 0.00 0.00 0.00 0.00 0.00 0.06 0.07 0.05 0.00 0.01 0.00 0.00
      X(矿物) 0.10 0.09 0.08 0.91 0.88 0.90 0.76 0.91 0.44 0.15 0.12 0.09 0.74 0.73 0.89 0.42 0.27 0.16
      Y(矿物) 0.29 0.24 0.22 0.10 0.08 0.09 0.12 0.14 0.14 0.08 0.07 0.06
      注:X(g)=Xpy=Mg/(Fe2++Mg+Ca);Y(g)=Xgr=Ca/(Fe2++Mg+Ca);X(hb)=角闪石M2位的Al;Y(hb)=角闪石的Ti含量;X(pl)=Ca/(Ca+Na)(L1903),X(pl)=Ca/(Ca+Na+K)(L1906);X(chl)=Mg/(Mg+Fe2+);g-C、g-R1、g-R2对应图 3的编号;矿物化学式的计算运用AX软件完成(https://filedn.com/lU1GlyFhv3UuXg5E9dbnWFF/TJBHpages/ax.html).
      下载: 导出CSV

      表  3  云中山地体石榴斜长角闪岩样品的锆石U-Pb定年结果

      Table  3.   Zircon U-Pb analytical results of garnet amphibolite samples from the Yunzhongshan terrane

      测点号 Th(10-6) U(10-6) Th/ U 同位素比值 年龄(Ma)
      207Pb/ 206Pb 207Pb/235U 206Pb/238U 207Pb/ 206Pb 206Pb/ 238U
      L1903
      1 0.22 32 0.007 0.113 5 0.004 6 5.144 0 0.215 5 0.327 9 0.004 6 1 857 74 1 828 22
      2 2.01 158 0.013 0.111 9 0.002 5 4.917 7 0.111 4 0.317 0 0.003 0 1 831 42 1 775 15
      3 0.95 144 0.007 0.110 4 0.002 9 4.917 0 0.131 1 0.320 3 0.003 4 1 806 44 1 791 17
      4 4.81 267 0.018 0.114 5 0.002 4 5.603 0 0.119 0 0.352 5 0.003 6 1 873 35 1 947 17
      L1906
      5 2.57 101 0.025 0.118 7 0.003 3 5.747 0 0.158 6 0.347 2 0.004 8 1 936 50 1 921 23
      6 0.44 86 0.005 0.114 2 0.003 1 5.703 4 0.175 8 0.357 1 0.005 5 1 933 50 1 968 26
      7 1.09 69 0.016 0.123 8 0.003 8 5.949 7 0.178 6 0.345 9 0.004 7 2 013 49 1 915 22
      8 2.43 195 0.012 0.122 5 0.003 2 5.598 9 0.144 0 0.328 3 0.003 5 1 994 46 1 830 17
      9 0.12 82 0.001 0.125 6 0.003 7 5.975 8 0.168 1 0.342 4 0.003 9 2 039 52 1 898 19
      10 0.08 41 0.002 0.116 7 0.004 0 5.635 8 0.194 7 0.347 5 0.004 3 1 907 62 1 923 21
      11 0.79 252 0.003 0.128 3 0.003 0 6.210 7 0.153 8 0.347 9 0.004 4 2 076 41 1 924 21
      12 0.50 69 0.007 0.120 9 0.003 3 5.715 4 0.149 9 0.340 9 0.003 2 1 970 48 1 891 15
      下载: 导出CSV
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