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    大兴安岭中段晚三叠世哈达陶勒盖组火山岩成因及构造背景

    马永非 刘永江 温泉波 张志斌 李伟 司秋亮 唐振

    马永非, 刘永江, 温泉波, 张志斌, 李伟, 司秋亮, 唐振, 2017. 大兴安岭中段晚三叠世哈达陶勒盖组火山岩成因及构造背景. 地球科学, 42(12): 2146-2173. doi: 10.3799/dqkx.2017.138
    引用本文: 马永非, 刘永江, 温泉波, 张志斌, 李伟, 司秋亮, 唐振, 2017. 大兴安岭中段晚三叠世哈达陶勒盖组火山岩成因及构造背景. 地球科学, 42(12): 2146-2173. doi: 10.3799/dqkx.2017.138
    Ma Yongfei, Liu Yongjiang, Wen Quanbo, Zhang Zhibin, Li Wei, Si Qiuliang, Tang Zhen, 2017. Petrogenesis and Tectonic Settings of Volcanic Rocks from Late Triassic Hadataolegai Fm. at Central Part of Great Xing'an Range. Earth Science, 42(12): 2146-2173. doi: 10.3799/dqkx.2017.138
    Citation: Ma Yongfei, Liu Yongjiang, Wen Quanbo, Zhang Zhibin, Li Wei, Si Qiuliang, Tang Zhen, 2017. Petrogenesis and Tectonic Settings of Volcanic Rocks from Late Triassic Hadataolegai Fm. at Central Part of Great Xing'an Range. Earth Science, 42(12): 2146-2173. doi: 10.3799/dqkx.2017.138

    大兴安岭中段晚三叠世哈达陶勒盖组火山岩成因及构造背景

    doi: 10.3799/dqkx.2017.138
    基金项目: 

    中国地质调查局地调项目 12120113053800

    科技部“973”项目 2013CB429802

    中国地质调查局地调项目 1212011120665

    中国地质调查局地调项目 D20160201-03

    详细信息
      作者简介:

      马永非(1986-), 男, 博士研究生, 主要从事构造地质研究

      通讯作者:

      刘永江

    • 中图分类号: P548

    Petrogenesis and Tectonic Settings of Volcanic Rocks from Late Triassic Hadataolegai Fm. at Central Part of Great Xing'an Range

    • 摘要: 为了解大兴安岭中段晚三叠世时期的构造背景,对该时期哈达陶勒盖组火山岩进行了岩石学、锆石U-Pb年代学及地球化学等方面的研究.哈达陶勒盖组火山岩可划分为中性系列安粗岩、安山岩,中酸性系列石英粗安岩及酸性系列流纹岩,形成年龄分别为:210.9±3.5 Ma、216.6±3.1 Ma、216.9±2.1 Ma和230.2±2.2 Ma.中性系列岩浆来源于原始地幔的部分熔融,并遭受俯冲板片释放流体的强烈富集作用.岩浆演化过程中结晶分异作用不明显,但遭受较强的地壳混染.中酸性系列和酸性系列岩浆来源于相对较浅的地壳物质深熔,前者岩浆演化过程中结晶分异作用较弱,而后者则较强.大兴安岭中段晚三叠世时期的构造演化背景受蒙古-鄂霍茨克洋板块向南俯冲作用的影响明显,在研究区表现为弧后伸展的构造背景.俯冲板片的断离拆沉引起了软流圈物质上涌,并导致伸展构造背景的形成,也为哈达陶勒盖组火山岩原始岩浆的形成提供了热量来源.

       

    • 图  1  (a) 中亚造山带及邻区构造简图;(b)东北地区构造格架图;(c)研究区地质图

      F1.新林-喜桂图缝合带;F2.贺根山-黑河缝合带;F3.索伦克尔-西拉木伦-长春缝合带;F4.依兰-伊通断裂;F5.敦化-密山断裂;F6.牡丹江断裂;a.根据Safonova and Santosh (2014)修改;b.根据Liu et al.(2017)Zhou and Wilde(2013)修改

      Fig.  1.  (a) Simplified tectonic framework of CAOB and surround areas; (b) Tectonic division of Northeast China; and (c) Detailed geological maps of study area

      图  2  晚三叠世哈达陶勒盖组火山岩典型岩石露头及显微照片

      a.安粗岩镜下照片:斑晶钾长石遭受明显的熔蚀及轻微碎裂;b.安山岩镜下照片:斑晶斜长石碎裂明显;c.石英粗安岩野外露头;d.石英粗安岩镜下照片;e.流纹岩野外露头;f.流纹岩镜下照片(斜长石及石英斑晶遭受明显熔蚀);Kfs.钾长石;PI.斜长石;Aug.普通辉石;Bt.黑云母;Qtz.石英

      Fig.  2.  Typical filed rock outcrops and its microscopic photomicrographs for the volcanic rocks from Late Triassic Hadataolegai Fm.

      图  4  晚三叠世哈达陶勒盖组火山岩U-Pb年龄谐和图

      Fig.  4.  U-Pb Concordia diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.

      图  3  晚三叠世哈达陶勒盖组火山岩典型锆石阴极发光(CL)图像

      Fig.  3.  Typical Cathodoluminescence (CL) images of selected zircon grains for the volcanic rocks from Late Triassic Hadataolegai Fm.

      图  5  晚三叠世哈达陶勒盖组火山岩主量元素图解

      a.(K2O+Na2O)-SiO2图解;b.(K2O+Na2O-CaO)-SiO2图解, 根据Frost et al.(2001)绘制;c.K2O-SiO2图解, 根据Peccerillo and Taylor(1976)绘制;d.A/KN-A/KNC图解, 根据Maniar and Piccoli(1989)绘制; A/CNK=分子数Al2O3/(Na2O+K2O+CaO),A/NK=分子数Al2O3/(Na2O+K2O)

      Fig.  5.  Major element diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.

      图  6  晚三叠世哈达陶勒盖组火山岩主量元素Harker图解

      TFeO= FeO+0.899 8Fe2O3

      Fig.  6.  Major element Harker diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.

      图  7  晚三叠世哈达陶勒盖组火山岩微量元素与SiO2含量协变图解

      Fig.  7.  Plots of various trace elements vs.SiO2 for the volcanic rocks from Late Triassic Hadataolegai Fm.

      图  8  晚三叠世哈达陶勒盖组火山岩球粒陨石标准化稀土元素配分模式图(a, c, e)和原始地幔标准化微量元素蛛网图(b, d, f)

      a, c, e.标准化值据Boynton(1984);b, d, f.标准值化据Sun and McDonough(1989)

      Fig.  8.  Chondrite-normalized rare earth element patterns (a, c, e) and Primitive mantle-normalized trace element spider diagrams (b, d, f) for the volcanic rocks from Late Triassic Hadataolegai Fm.

      图  9  晚三叠世哈达陶勒盖组火山岩

      a.Sm/Yb-Sm图解;b.La/Ba-La/Nb图解;c.Th/Y-Sm/Th图解;d.Ba/Th-(La/Sm)N图解;其中图a中分别由原始地幔及亏损地幔为源区的尖晶石二辉橄榄岩(Ol0.53+Opx0.27+Cpx0.17+Sp0.13)及石榴石二辉橄榄岩(Ol0.60+Opx0.20+Cpx0.10+Gt0.10)熔融曲线根据Aldanmaz et al.(2000)Zhao and Zhou(2007b, 2009)的数据模式绘制.实线代表由原始地幔熔融的曲线,虚线代表由亏损地幔熔融的曲线,各熔融曲线上短线段旁的数字代表熔融程度;DM.亏损地幔(McKenzie and O'Nions,1991);PM.原始地幔(Sun and McDonough, 1989);HIMU.高U/Pb比值地幔源区(Saunders et al., 1992);MORB.大洋中脊玄武岩源区;OIB.洋岛玄武岩源区(Sun and McDonough, 1989);CLM.大陆岩石圈地幔(Sun and McDonough, 1989);N-MORB.正常的大洋中脊玄武岩(Sun and McDonough, 1989)

      Fig.  9.  The volcanic rocks from Late Triassic Hadataolegai Fm.

      图  10  晚三叠世哈达陶勒盖组火山岩岩石类型判别图解

      a.[(K2O+Na2O)/CaO]-(Zr+Nb+Ce+Y)图解;b.(TFeO/MgO)-(Zr+Nb+Ce+Y)图解;a和b据Whalen et al.(1987)绘制

      Fig.  10.  Diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.with rock type discrimination purpose

      图  11  晚三叠世哈达陶勒盖组火山岩

      a.(La/Yb)N-YbN图解,跟据Drummond and Defant(1990);b.Sr/Y-Y图解,跟据Martin(1999)

      Fig.  11.  Diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.

      图  12  晚三叠世哈达陶勒盖组火山岩图解

      a.Hf/3-Th-Nb/16图解,跟据Wood(1980);b.Rb-Y+Nb图解,跟据Pearce et al.(1984)

      Fig.  12.  Diagrams for the volcanic rocks from Late Triassic Hadataolegai Fm.

      图  13  大兴安岭中段地区晚三叠世哈达陶勒盖组火山岩成因模式及构造背景简图

      Fig.  13.  Schematic diagram showing the petrogenetic model and tectonic background for the volcanic rocks from Late Triassic Hadataolegai Fm.at central Great Xing'an Rang

      表  1  晚三叠世哈达陶勒盖组火山岩主量(wt%)、稀土和微量元素(10-6)分析结果

      Table  1.   Major (wt%) and trace elements (10-6) analysis result of the volcanic rocks from Late Triassic Hadataolegai Fm.

      样号中性系列中酸性系列酸性系列
      PM305-5-1YQTC303Q1TC106Q2TC107Q2TC125YQ1PM101-18-1QPM302-1-1QPM206-13-1YQPM209-5-1YQPM209-7-1YQPM206-37-1YQPM208-9-1YQTC128YQ1t1106YQ3
      SiO255.8655.9853.5960.1756.2657.2861.4466.1867.4267.5170.6079.3772.9275.60
      TiO21.171.121.190.800.921.000.690.760.590.610.350.140.360.13
      Al2O317.4118.0617.5116.8517.8217.2015.8516.3315.5215.1014.4710.8514.3812.58
      Fe2O35.527.425.792.923.564.573.413.611.841.292.741.091.731.20
      FeO1.281.714.043.234.363.552.560.760.811.170.310.220.670.56
      TFeO6.258.399.255.867.577.665.634.012.472.332.781.202.231.64
      MnO0.080.130.130.090.110.130.090.040.060.080.070.010.030.02
      MgO2.171.684.054.244.423.212.960.600.560.790.480.020.471.66
      CaO5.291.996.372.564.525.725.061.421.061.531.400.430.430.29
      Na2O5.846.104.444.333.864.494.314.635.564.703.361.663.083.98
      K2O2.302.211.742.141.401.922.924.634.764.865.125.494.573.21
      P2O50.420.410.440.310.320.310.230.210.130.160.150.060.110.03
      LOI1.633.611.092.363.110.870.550.990.850.961.060.591.270.93
      Total98.97100.41100.3799.99100.66100.23100.07100.1699.1798.75100.1099.93100.03100.18
      K2O+
      Na2O8.378.586.226.635.396.457.269.3410.509.788.567.207.757.24
      A/CNK0.801.120.851.191.110.870.821.070.950.951.061.141.321.18
      La39.4628.1621.3527.6319.8720.7124.7339.7343.7742.8430.8017.1434.9823.21
      Ce84.9071.1643.9355.9940.2643.3848.4881.4189.8588.4461.7635.7265.9547.83
      Pr11.598.456.577.685.466.466.4210.5811.7111.337.164.477.586.43
      Nd46.8234.8828.2131.0824.1927.6225.4342.8143.9842.5826.3618.2328.1427.12
      Sm8.056.935.465.534.855.384.458.118.057.854.564.004.845.91
      Eu2.472.131.772.171.472.112.111.672.111.920.740.590.871.26
      Gd6.085.204.524.433.724.513.776.356.896.493.533.363.985.10
      Tb0.800.700.660.550.570.680.501.011.031.000.570.660.630.91
      Dy4.073.633.502.642.693.612.605.086.246.012.973.743.255.37
      Ho0.680.670.680.500.590.720.481.001.141.100.560.880.681.19
      Er1.751.831.661.241.591.841.262.803.063.031.772.642.022.92
      Tm0.270.250.280.210.250.320.200.490.530.530.330.500.380.51
      Yb1.601.751.711.321.521.991.283.113.353.422.403.272.383.95
      Lu0.210.230.240.190.240.280.170.480.470.500.360.540.360.53
      Y16.4916.8819.4015.6612.9720.4812.7125.7229.7428.3017.2223.5518.4531.20
      ΣREE208.75165.97120.55141.15107.25119.62121.88204.63222.17217.05143.8695.73156.03132.23
      (La/Yb)N17.6411.558.9614.979.417.4813.879.179.379.009.223.7610.544.22
      δEu1.041.041.061.291.021.281.530.690.850.800.540.480.590.69
      Li9.6572.168.0319.7633.025.568.4517.3113.2518.5217.712.7421.4711.94
      Be1.464.570.841.281.240.840.942.312.512.882.230.871.811.30
      Th5.6110.326.5916.108.8012.049.2710.928.2211.4811.237.906.947.28
      U1.181.890.792.440.821.071.753.602.494.053.481.932.622.37
      Hf4.545.353.745.099.965.786.0312.238.619.749.884.715.516.09
      Ta0.250.490.310.630.370.460.331.050.340.721.220.920.991.02
      Sc13.1219.7113.299.7813.8411.889.676.737.726.963.444.185.137.45
      Ba8298275501 1004606638821 0561 1621 1031 0451 417769772
      Nb3.358.286.396.394.306.446.2911.2415.3315.1210.699.119.529.97
      Rb3163334124335611699120129778465
      Sr181496093777899579870638429536024610930874
      Zr150185119177147166162409403418245166236213
      Co20.8131.6622.7419.0527.2119.4615.828.575.006.097.704.636.000.91
      V148.0161.4176.893.0112.7133.993.239.731.838.723.312.431.117.6
      (La/Sm)N3.172.622.533.222.652.483.593.163.513.524.362.774.672.54
      Ba/Th147.780.1183.3968.3352.2955.0895.1696.71141.3896.0693.11179.26110.75105.97
      La/Nb11.783.403.344.324.623.223.933.532.862.832.881.883.672.33
      La/Ba0.050.030.040.030.040.030.030.040.040.040.030.010.050.03
      Sm/Yb5.013.963.194.183.202.713.482.612.402.301.901.222.031.50
      Sm/Th1.430.670.830.340.550.450.480.740.980.680.410.510.700.81
      Th/Y0.340.610.341.030.680.590.730.420.280.410.650.340.380.23
      下载: 导出CSV

      表  2  晚三叠世哈达陶勒盖组火山岩LA-ICP-MS锆石U-Pb测年数据

      Table  2.   LA-ICP-MS Zircon U-Pb data for the volcanic rocks from Late Triassic Hadataolegai Fm.

      测点号Th/U同位素比值同位素年龄(Ma)
      207Pb/206Pb±1δ206Pb/238U±1δ207Pb/235U±1δ207Pb/206Pb±1δ206Pb/238U±1δ207Pb/235U±1δ
      DH2011RZ11:安粗岩
      DH2011RZ11_30.670.058 10.003 40.031 00.000 80.227 30.014 8532123197520812
      DH2011RZ11_50.750.049 70.001 70.032 80.000 70.230 40.008 61807820842117
      DH2011RZ11_70.850.051 80.002 10.033 40.000 70.239 00.011 02779221252189
      DH2011RZ11_90.840.051 50.001 60.032 70.000 70.235 70.008 12647120842157
      DH2011RZ11_100.960.052 10.001 50.033 20.000 70.233 00.006 92886221142136
      DH2011RZ11_120.690.054 00.002 10.035 30.000 80.243 20.010 23718322352218
      DH2011RZ11_130.800.051 60.001 40.036 00.000 70.254 60.007 12675922842306
      DH2011RZ11_151.590.051 40.001 30.031 30.000 60.224 50.006 12615819942065
      DH2011RZ11_170.760.053 70.002 30.031 30.000 70.222 00.010 53609319942049
      DH2011RZ11_180.890.049 60.001 90.032 90.000 70.225 10.009 71778820842068
      DH2011RZ11_190.970.051 50.001 70.034 20.000 70.255 20.009 42657521742318
      DH2011RZ11_200.880.048 00.001 80.033 20.000 70.214 60.008 8978821141977
      DH2011RZ11_220.650.052 90.001 70.034 00.000 70.243 30.008 33237021642217
      DH2011RZ11_230.890.049 40.001 70.033 80.000 70.228 90.008 51657821542097
      DH2011RZ11_241.240.050 80.001 80.032 30.000 70.236 30.009 22318020542158
      DH2011RZ11_260.790.055 00.001 40.032 10.000 60.233 70.006 44105720442135
      DH2011RZ11_270.850.051 40.001 40.033 20.000 70.234 00.006 62596121042145
      DH2011RZ11_280.770.050 70.001 60.034 10.000 70.239 90.008 32267221642187
      DH2011RZ11_290.940.048 90.001 40.033 00.000 70.223 80.006 81436620942056
      DH2011RZ11_300.820.049 60.001 40.033 20.000 70.230 00.007 11786621142106
      DH2011RZ11_340.570.049 40.001 80.034 30.000 70.227 20.009 01668221842087
      DH2011RZ11_350.700.050 40.001 60.035 10.000 70.244 30.008 22127122342227
      DH2011RZ17:安山岩
      DH2011RZ17_10.740.051 00.001 40.033 60.000 70.242 30.007 22426321342206
      DH2011RZ17_20.870.052 60.001 60.034 40.000 70.246 40.008 23136821842247
      DH2011RZ17_30.770.052 20.001 50.034 80.000 70.252 30.008 12936622142287
      DH2011RZ17_40.870.051 60.001 70.034 50.000 70.236 70.008 42677321942167
      DH2011RZ17_50.810.051 00.001 50.035 50.000 70.252 40.008 12396622552297
      DH2011RZ17_60.770.050 20.002 20.032 10.000 70.218 30.010 920510120452019
      DH2011RZ17_70.810.049 70.001 60.033 20.000 70.233 60.008 41817521142137
      DH2011RZ17_81.140.052 40.001 20.032 40.000 60.229 80.005 73015320642105
      DH2011RZ17_90.950.050 20.001 30.032 90.000 70.230 60.006 52066120942115
      DH2011RZ17_110.790.050 30.001 30.035 70.000 70.251 20.006 82095822642285
      DH2011RZ17_130.660.050 00.001 60.034 30.000 70.240 30.008 41957321842197
      DH2011RZ17:安山岩
      DH2011RZ17_150.880.049 80.001 30.033 40.000 70.232 90.006 41886021242135
      DH2011RZ17_170.780.051 60.001 40.036 30.000 70.255 60.007 12685923042316
      DH2011RZ17_180.720.052 00.001 70.032 80.000 70.231 60.008 02847120842127
      DH2011RZ17_190.770.049 90.001 80.033 60.000 70.236 80.009 11918021342168
      DH2011RZ17_200.680.052 90.001 50.035 20.000 70.248 70.007 73236422342266
      DH2011RZ17_220.780.051 40.001 40.034 10.000 70.244 30.007 02596121642226
      DH2011RZ17_230.630.048 60.003 10.033 70.000 90.228 20.016 4127142214620914
      DH2011RZ17_240.670.051 20.001 80.034 80.000 70.249 70.009 62497822152268
      DH2011RZ17_250.760.053 80.001 80.036 90.000 80.256 90.009 23637223352327
      DH2011RZ17_260.780.049 30.001 70.033 80.000 70.225 10.008 51627921442067
      DH2011RZ17_290.940.054 90.001 80.033 70.000 70.244 20.008 84087121442227
      DH2011RZ17_300.870.050 10.001 80.035 10.000 80.244 00.009 82018222252228
      DH2011RZ17_320.790.049 50.001 60.034 30.000 70.237 60.008 31717321742167
      TW04:石英粗安岩
      TW04_31.940.050 50.001 30.035 00.000 80.246 30.006 62175722252245
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