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    吉林省辽源晚中生代碱性玄武岩成因及岩石圈地幔性质

    路思明 裴福萍 周群君 靳克 彭玉鲸 陈岩 许文良

    路思明, 裴福萍, 周群君, 靳克, 彭玉鲸, 陈岩, 许文良, 2012. 吉林省辽源晚中生代碱性玄武岩成因及岩石圈地幔性质. 地球科学, 37(3): 475-488. doi: 10.3799/dqkx.2012.054
    引用本文: 路思明, 裴福萍, 周群君, 靳克, 彭玉鲸, 陈岩, 许文良, 2012. 吉林省辽源晚中生代碱性玄武岩成因及岩石圈地幔性质. 地球科学, 37(3): 475-488. doi: 10.3799/dqkx.2012.054
    LU Si-ming, PEI Fu-ping, ZHOU Qun-jun, JIN Ke, PENG Yu-jing, CHEN Yan, XU Wen-liang, 2012. Origin of Late Mesozoic Alkaline Basalts and Nature of Lithospheric Mantle in Liaoyuan Area, Jilin Province. Earth Science, 37(3): 475-488. doi: 10.3799/dqkx.2012.054
    Citation: LU Si-ming, PEI Fu-ping, ZHOU Qun-jun, JIN Ke, PENG Yu-jing, CHEN Yan, XU Wen-liang, 2012. Origin of Late Mesozoic Alkaline Basalts and Nature of Lithospheric Mantle in Liaoyuan Area, Jilin Province. Earth Science, 37(3): 475-488. doi: 10.3799/dqkx.2012.054

    吉林省辽源晚中生代碱性玄武岩成因及岩石圈地幔性质

    doi: 10.3799/dqkx.2012.054
    基金项目: 

    吉林省科技发展计划项目 20080454

    国家自然科学基金项目 40872049

    吉林大学科学前沿与交叉学科创新项目 200903032

    详细信息
      作者简介:

      路思明(1987-), 女, 硕士研究生, 矿物学、岩石学、矿床学专业

      通讯作者:

      裴福萍, E-mail: peifp@jlu.edu.cn

    • 中图分类号: P581

    Origin of Late Mesozoic Alkaline Basalts and Nature of Lithospheric Mantle in Liaoyuan Area, Jilin Province

    • 摘要: 报道了吉林辽源晚中生代玄武岩的全岩K-Ar定年结果和岩石地球化学资料, 以及其中幔源捕虏体的矿物化学分析结果, 探讨了晚中生代碱性玄武岩的成因及岩石圈地幔的性质.全岩K-Ar定年结果显示, 辽源玄武岩形成于晚白垩世(91.7±1.7 Ma、82.5±1.9 Ma、99.3±1.6 Ma、82.2±2.4 Ma).该玄武岩的SiO2含量介于45.1%~45.9%之间, 全碱(Na2O+K2O)含量介于4.50%~6.72%之间, Mg#[100×Mg/(Mg+Fe2+)]值介于60~63之间, 属于碱性玄武岩系列.该玄武岩相对富集轻稀土元素(LREEs)、亏损重稀土元素(HREEs), (La/Yb)N值介于12.0~14.0之间, 无Eu异常, 具有洋岛玄武岩(OIB)型微量元素配分型式.辽源玄武岩中的幔源捕虏体以尖晶石二辉橄榄岩为主, 捕虏体中橄榄石的Mg#值较低(87.1~91.2), 结合捕虏体中其他矿物的主量和微量元素地球化学特征, 认为辽源晚白垩世岩石圈地幔以新增生的岩石圈地幔为主.捕虏体中单斜辉石的LREEs具有从富集到亏损的变化特征, 暗示岩石圈地幔经历了部分熔融和交代作用的改造, 地幔交代类型以硅酸盐熔体交代为主, 同时存在碳酸盐熔体交代作用.辽源晚白垩世玄武岩来源于软流圈地幔的部分熔融, 结合区域研究成果, 认为辽源晚白垩世玄武岩形成于古太平洋板块俯冲背景下的弧后伸展环境.

       

    • 图  1  辽源玄武岩地质简图

      Fig.  1.  Simplified geological map of Liaoyuan basalts

      图  2  玄武岩和橄榄岩捕虏体的产状与结构

      a.橄榄岩捕虏体的野外产状;b.玄武岩的斑状结构(正交偏光);c.捕虏体的结构(正交偏光);d.捕虏体中矿物特征(单偏光).Cpx.透辉石;Ol.橄榄石;Opx.斜方辉石;Sp.尖晶石

      Fig.  2.  Field photographs and photomicrographs showing the occurrence of lherzolite xenoliths and texture of basalts

      图  3  辽源晚白垩世玄武岩的TAS图解

      阴影区为延边晚白垩世火山岩的分布范围;大屯玄武岩数据张辉煌等(2006);延边火山岩数据引自Ji et al.(2007);华北克拉通晚白垩世玄武岩数据许文良等(1999)张宏福和郑建平(2003)王微等(2006);碱性和亚碱性系列之间的界限引自Irvine and Baragar(1971)

      Fig.  3.  Total alkali vs. SiO2 variation diagram for the Liaoyuan basalts

      图  4  辽源玄武岩稀土元素和微量元素配分图解

      华北克拉通玄武岩数据王冬艳等(2002)张宏福和郑建平(2003)、闫峻等(2005)和王微等(2006);大屯数据张辉煌等(2006);延边火山岩数据引自Ji et al.(2007);球粒陨石标准化数据引自Boynton(1984);原始地幔标准化数据和洋岛玄武岩(OIB)数据引自Sun and McDonough(1989)

      Fig.  4.  Chondrite-normalized REE patterns and primitive mantle-normalized trace element spidergrams for Liaoyuan basalts

      图  5  辽源橄榄岩捕虏体中单斜辉石稀土元素配分图解(a,c,e)和微量元素蛛网图(b,d,f)

      球粒陨石标准化数据引自Boynton(1984);原始地幔标准化数据引自Sun and McDonough(1989);C.矿物核部;R.矿物边部

      Fig.  5.  Chondrite-normalized REE patterns (a, c, e) and primitive mantle-normalized trace element spidergrams (b, d, f) of clinopyroxenes from the peridotite xenoliths entrained by Liaoyuan basalts

      图  6  辽源玄武岩中橄榄岩捕虏体单斜辉石的Ti/Eu与(La/Yb)N图解

      Grande Comore和Samoa地区数据引自Coltorti et al.(1999);阜新和大西庄数据王微(2008)

      Fig.  6.  Ti/Eu versus (La/Yb)N for clinopyroxenes from peridotite xenoliths entrained by the Liaoyuan basalts

      表  1  辽源玄武岩全岩K-Ar同位素定年结果

      Table  1.   Whole-rock K-Ar isotope dating result of the Liaoyuan Basalts

      样品号 年龄(Ma) ± K(%) 权重(g) Exp Serial Radiogenic 40Ar 38Ar(10-11 mol) 40Ar/38Ar 40Ar/38Ar(±) 36Ar/38Ar 36Ar/38Ar(±) 40Ar*/40K 40Ar*/40K(±)
      (mol/g) (%)
      JL1-14 91.70 1.67 0.76 0.079 7 3 446 1.24E-10 36.14 2.09E-11 1.309 809 0.000 27 0.002 882 6.65E-06 0.005 465 0.000 102
      JL2-3 82.55 1.94 1.76 0.060 4 3 445 2.58E-10 60.77 2.09E-11 1.227 719 0.006 39 0.001 661 3.83E-06 0.004 908 0.000 118
      JL4-2 99.28 1.59 1.36 0.061 3 3 444 2.41E-10 52.67 2.09E-11 1.342 086 0.000 218 0.002 189 5.27E-06 0.005 930 0.000 098
      JL7-3 82.18 2.37 0.93 0.061 5 3 442 1.36E-10 45.04 2.09E-11 0.887 004 0.002 483 0.001 681 1.27E-05 0.004 885 0.000 144
      下载: 导出CSV

      表  2  辽源玄武岩主量元素(%)和微量元素(10-6)分析结果

      Table  2.   Major (%) and trace element (10-6) data of the Liaoyuan basalts

      样品编号 SiO2 TiO2 Al2O3 Fe2O3 MnO MgO CaO Na2O K2O P2O5 LOI 总量 Mg# Na2O/K2O
      JL1-14 45.4 2.37 15.7 9.92 0.16 7.82 8.76 3.68 0.82 0.60 4.52 99.4 61 4.49
      JL2-3 45.9 2.26 16.0 8.83 0.14 6.61 7.15 4.37 2.35 0.72 5.36 99.4 60 1.86
      JL4-2 45.1 2.34 15.1 10.22 0.15 8.92 8.65 2.95 1.76 0.58 3.98 99.5 63 1.68
      JL7-3 45.6 2.28 15.8 9.9 0.15 7.77 8.64 4.00 1.12 0.66 3.92 99.5 61 3.59
      样品编号 Li Be Sc V Cr Co Ni Cu Zn Ga Rb Sr Y Zr
      JL1-14 10.0 1.76 24.5 243 166 42.6 200 36.4 70.4 18.5 14.1 787 28.4 200
      JL2-3 6.89 2.03 20.1 199 127 34.5 128 37.6 70.8 18.5 60.5 946 28.8 245
      JL4-2 7.61 1.42 23.3 231 199 44.3 219 61.8 73.2 18.4 51.3 837 26.1 191
      JL7-3 9.68 1.89 24.6 233 162 40.8 169 52.0 76.0 19.1 36.5 920 28.6 223
      样品编号 Nb Mo Cs Ba La Ce Pr Nd Sm Eu Gd Tb Dy Ho
      JL1-14 65.3 1.76 1.04 902 41.0 76.0 8.94 35.6 7.37 2.24 6.42 0.91 5.34 0.98
      JL2-3 78.6 1.89 0.89 1104 50.1 91.2 10.5 40.4 8.13 2.48 6.85 0.97 5.57 1.02
      JL4-2 63.5 1.58 0.69 863 38.7 71.6 8.55 33.1 7.01 2.20 6.30 0.87 5.15 0.95
      JL7-3 75.0 1.84 0.88 1074 47.1 86.4 10.0 39.0 7.96 2.44 7.03 0.95 5.52 1.03
      样品编号 Er Tm Yb Lu Hf Ta Pb Th U Sr/Y (La/Yb)N δEu ΣREE
      JL1-14 2.57 0.37 2.31 0.33 4.60 3.71 3.37 5.79 1.33 27.7 12.0 0.97 190
      JL2-3 2.58 0.37 2.40 0.35 5.26 4.36 4.15 7.12 1.64 32.9 14.0 0.99 223
      JL4-2 2.49 0.34 2.14 0.32 4.38 3.50 2.96 5.27 1.25 32.1 12.2 1.00 180
      JL7-3 2.65 0.36 2.43 0.34 4.83 4.10 3.79 6.49 1.49 32.1 13.1 0.98 213
      注:Mg#=100×Mg2+/(Mg2++Fe2+);(La/Yb)N球粒陨石标准化数据采用Boynton(1984).
      下载: 导出CSV

      表  3  辽源地幔橄榄岩捕虏体中矿物的主量元素(%)和微量元素(10-6) 分析结果

      Table  3.   Major-, trace-element (10-6) data of the composed minerals from the peridotite xenoliths carried by the Liaoyuan basalts

      捕虏体类型 尖晶石二辉橄榄岩
      样品号 JL1-3 JL1-4 JL1-12
      矿物 Ol Cpx Opx Ol Ol Cpx Opx Sp
      打点位置 R C C C R C C R R M R C C C R C R C C C
      SiO2 39.9 39.9 39.6 50.7 55.1 55.1 54.2 40.7 41.9 42.2 40.8 40.9 41.3 41.6 51.7 51.6 56.4 56.5 0.26 0.26
      TiO2 0.01 0.00 0.00 0.33 0.10 0.09 0.10 0.02 0.00 0.01 0.00 0.00 0.01 0.00 0.67 0.68 0.16 0.17 0.16 0.16
      Al2O3 0.02 0.02 0.02 6.09 4.36 4.34 4.57 0.14 0.11 0.07 0.03 0.02 0.01 0.02 6.08 6.10 4.30 4.30 52.7 53.4
      TFeO 10.8 10.9 10.6 3.46 6.86 6.81 6.92 13.7 9.65 10.6 9.94 9.83 10.9 10.5 3.11 3.12 6.25 6.20 14.4 13.6
      MnO 0.18 0.17 0.16 0.10 0.15 0.15 0.15 0.44 0.14 0.21 0.15 0.15 0.19 0.18 0.09 0.09 0.14 0.14 0.14 0.13
      MgO 48.6 48.6 49.1 16.5 31.7 31.8 32.2 44.6 47.5 46.3 48.6 48.6 47.1 47.3 15.3 15.2 31.2 31.2 22.6 22.6
      CaO 0.11 0.08 0.09 20.4 1.01 0.97 1.03 0.19 0.17 0.19 0.07 0.08 0.14 0.10 20.8 21.0 0.93 0.94 0.00 0.01
      Na2O 0.01 0.01 0.01 1.28 0.10 0.11 0.11 0.01 0.03 0.01 0.01 0.01 0.01 0.01 1.48 1.46 0.11 0.12 0.00 0.00
      K2O 0.00 0.00 0.00 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 0.00 0.00 0.00
      P2O5 0.01 0.01 0.01 0.01 0.01 0.01 0.01 0.02 0.02 0.02 0.02 0.02 0.02 0.02 0.02 0.02 0.01 0.01 0.00 0.01
      总量 99.6 99.6 99.6 98.9 99.4 99.4 99.3 99.7 99.6 99.6 99.6 99.6 99.7 99.7 99.2 99.2 99.5 99.5 90.2 90.2
      Mg# 88.9 88.9 89.2 89.5 89.2 89.3 89.3 85.4 89.8 88.7 89.7 89.8 88.6 89.0 89.8 89.7 91.7 91.7 73.7 74.8
      Cr# 55.1 47.8 35.4 9.91 7.04 7.06 7.10 4.94 26.9 28.9 18.0 26.0 31.3 30.1 6.80 6.57 5.15 5.00 10.4 10.3
      Cr 213 176 132 6 831 3 365 3 359 3 562 74 417 280 73 67 52 67 4 525 4 372 2 379 2 308 62 237 62 527
      Ni 2 730 2 886 3 010 384 785 782 817 1 583 2 718 2 427 2 570 2 530 2 240 2 305 292 291 656 649 3 088 3 122
      捕虏体类型 尖晶石二辉橄榄岩 纯橄榄岩
      样品号 JL1-13 JL7-2 JL2-2 JL4-2
      矿物 Ol Cpx Opx Ol Cpx Opx Ol Opx Sp Ol
      打点位置 R C R C R C C C C C C R R C C R C R R
      SiO2 40.8 41.6 54.6 54.2 57.6 56.9 41.5 51.8 55.7 39.0 39.3 37.7 54.8 54.7 0.92 37.4 38.0 37.6 37.0
      TiO2 0.00 0.00 0.09 0.10 0.07 0.04 0.00 0.46 0.10 0.00 0.00 0.00 0.03 0.03 0.76 0.01 0.02 0.01 0.01
      Al2O3 0.01 0.02 2.96 3.00 2.60 2.58 0.02 6.24 4.54 0.01 0.01 0.01 2.96 2.96 32.7 0.07 0.14 0.06 0.05
      TFeO 10.8 10.3 3.06 3.15 6.53 6.72 9.35 2.71 6.13 9.05 8.86 18.0 6.10 6.02 23.4 15.0 12.8 14.8 18.9
      MnO 0.17 0.15 0.09 0.09 0.15 0.15 0.14 0.08 0.14 0.15 0.14 0.36 0.14 0.14 0.26 0.24 0.19 0.25 0.36
      MgO 47.7 47.5 16.1 16.3 31.1 31.6 48.5 15.0 32.0 51.3 51.2 43.6 34.4 34.6 15.0 46.7 48.3 46.6 43.1
      CaO 0.12 0.09 20.8 20.8 1.06 1.06 0.08 21.7 0.88 0.07 0.07 0.14 0.88 0.87 0.01 0.26 0.28 0.30 0.35
      Na2O 0.01 0.01 1.05 1.07 0.11 0.10 0.01 1.38 0.10 0.00 0.00 0.01 0.02 0.02 0.00 0.01 0.03 0.01 0.01
      K2O 0.00 0.00 0.00 0.01 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.00 0.01 0.00 0.01 0.00 0.00
      P2O5 0.04 0.02 0.02 0.02 0.01 0.01 0.01 0.01 0.00 0.01 0.01 0.02 0.00 0.00 0.00 0.01 0.02 0.01 0.02
      总量 99.6 99.6 98.8 98.7 99.2 99.2 99.6 99.3 99.6 99.6 99.6 99.8 99.3 99.3 73.0 99.7 99.7 99.7 99.7
      Mg# 88.8 88.8 90.4 90.2 89.5 89.4 90.3 90.8 90.3 91.0 91.2 81.3 91.0 91.1 53.5 84.8 87.1 84.9 80.3
      Cr# 52.0 49.4 19.9 19.9 14.3 14.8 23.0 6.19 4.19 40.1 46.9 20.0 10.7 10.7 35.1 20.6 14.6 25.6 18.8
      Cr 162 154 7 507 7 604 4 402 4 574 52 4 195 2 027 89 117 35 3 614 3 605 180 523 180 241 210 129
      Ni 2 856 2 747 339 357 748 798 2 696 301 730 2 932 2 947 1 614 766 739 1 781 1 756 1 919 1 852 1 573
      注:Ol.橄榄石;Cpx.单斜辉石;Opx.斜方辉石;Sp.尖晶石;C.核部;M.幔部;R.边部;Mg#=100×Mg2+/(Mg2++Fe2+);Cr#=100×Cr3+/(Cr3++Al3+).
      下载: 导出CSV

      表  4  橄榄岩捕虏体中单斜辉石微量元素(10-6)分析结果

      Table  4.   Trace-element (10-6) data of clinopyroxenes from the xenoliths

      样品号 Sc V Cr Co Ni Cu Zn Ga Rb Sr Y Zr Nb Cs Ba Hf Ta Pb Th U Sr/Y
      JL1-13-R 73.7 249 7 507 21.8 339 1.11 17.5 2.37 0.01 223 5.3 38.9 1.48 0 0.26 0.85 0.2 0.1 0.34 0.05 41.9
      JL1-13-C 73.8 246 7 604 22.4 357 1.31 16.9 2.51 0.13 207 5.4 40.3 1.76 0 0.71 0.78 0.21 0.14 0.36 0.07 38.0
      JL1-12-R 63.7 296 4 525 20.3 292 1.43 11.5 4.08 0.02 42 17.8 34.0 0.30 0 0.19 1.16 0.03 0.46 0.12 0.03 2.39
      JL1-12-C 64.8 301 4 372 20.2 291 1.65 12.7 4.08 0.01 47 18.0 32.8 0.29 0 0.03 1.11 0.03 0.12 0.11 0.04 2.59
      JL1-3-C 63.9 266 6 831 23.3 384 1.66 13.5 3.78 0.15 60 13.2 11.1 1.09 0 7.64 0.52 0.04 0.04 0.15 0.03 4.53
      JL7-2-C 70.2 271 4 195 19.7 301 2.07 11.5 3.34 0.09 34 19.0 22.0 0.10 0.01 0.44 0.89 0.01 0.25 0.02 0.01 1.77
      样品号 La Ce Pr Nd Sm Eu Gd Tb Dy Ho Tm Yb Lu (La/Yb)N δEu ΣREE
      JL1-13-R 9.81 26.0 3.02 12.03 2.32 0.66 1.63 0.20 1.06 0.21 0.07 0.55 0.07 12.03 0.99 57.7
      JL1-13-C 9.45 24.4 2.88 11.35 2.21 0.62 1.68 0.20 1.11 0.21 0.08 0.48 0.06 13.27 0.95 54.7
      JL1-12-R 1.71 5.27 0.87 4.39 1.68 0.67 2.24 0.43 3.20 0.71 0.27 1.94 0.27 0.59 1.06 23.7
      JL1-12-C 1.86 5.51 0.85 4.55 1.84 0.70 2.51 0.49 3.47 0.71 0.28 1.76 0.27 0.71 1.00 24.8
      JL1-3-C 1.60 2.48 0.31 1.74 0.89 0.39 1.66 0.3 2.28 0.51 0.20 1.20 0.19 0.90 0.97 13.8
      JL7-2-C 0.19 1.36 0.34 2.78 1.3 0.65 2.54 0.47 3.52 0.74 0.30 1.91 0.29 0.07 1.07 16.4
      注:Mg#=100×Mg2+/(Mg2++Fe2+);(La/Yb)N球粒陨石标准化数据采用Boynton(1984).
      下载: 导出CSV
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