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    内蒙古巴林右旗巴彦查干岩体年代学与地球化学:对古亚洲洋闭合时间的限定

    杜继宇 陶楠 郭建超 江斌 杜贯新

    杜继宇, 陶楠, 郭建超, 江斌, 杜贯新, 2019. 内蒙古巴林右旗巴彦查干岩体年代学与地球化学:对古亚洲洋闭合时间的限定. 地球科学, 44(10): 3361-3377. doi: 10.3799/dqkx.2019.215
    引用本文: 杜继宇, 陶楠, 郭建超, 江斌, 杜贯新, 2019. 内蒙古巴林右旗巴彦查干岩体年代学与地球化学:对古亚洲洋闭合时间的限定. 地球科学, 44(10): 3361-3377. doi: 10.3799/dqkx.2019.215
    Du Jiyu, Tao Nan, Guo Jianchao, Jiang Bin, Du Guanxin, 2019. Geochronology and Geochemistry of Bayanchagan Pluton in Balinyouqi, Inner Mongolia: Implication for Timing of Closure of Paleo-Asian Ocean. Earth Science, 44(10): 3361-3377. doi: 10.3799/dqkx.2019.215
    Citation: Du Jiyu, Tao Nan, Guo Jianchao, Jiang Bin, Du Guanxin, 2019. Geochronology and Geochemistry of Bayanchagan Pluton in Balinyouqi, Inner Mongolia: Implication for Timing of Closure of Paleo-Asian Ocean. Earth Science, 44(10): 3361-3377. doi: 10.3799/dqkx.2019.215

    内蒙古巴林右旗巴彦查干岩体年代学与地球化学:对古亚洲洋闭合时间的限定

    doi: 10.3799/dqkx.2019.215
    基金项目: 

    中国地质调查局项目 DD20160048-02

    中国地质调查局项目 DD20190039

    中国地质调查局项目 DD20160048-01

    中国地质调查局项目 DD20190042

    中国地质调查局项目 DD20190039-06

    中国地质调查局项目 DD20190360

    中国地质调查局项目 12120115031101

    详细信息
      作者简介:

      杜继宇(1988—), 男, 在职博士研究生, 工程师, 主要从事大兴安岭地区构造地质及岩石地球化学研究

      通讯作者:

      陶楠(1982—), 男, 高级工程师

    • 中图分类号: P597

    Geochronology and Geochemistry of Bayanchagan Pluton in Balinyouqi, Inner Mongolia: Implication for Timing of Closure of Paleo-Asian Ocean

    • 摘要: 古亚洲洋闭合时限一直存在争议.对巴林右旗巴彦查干岩体进行了地球化学、锆石U-Pb测年和Lu-Hf同位素研究,确定其时代和成因,探讨区域构造背景.巴彦查干岩体岩性为二云母二长花岗岩.测年显示,花岗岩侵位于232.0~241.7 Ma,为中晚三叠世.花岗岩富硅和铝,贫镁和铁,属强过铝系列(A/CNK=1.10~1.25),富集轻稀土和大离子亲石元素,亏损重稀土和Nb、Ta等高场强元素,具S型花岗岩特征.锆石的εHft)值为-1.8~+4.01,二阶段模式年龄(tDM2)在1 006~1 380 Ma之间.上述研究表明,原始岩浆起源于加厚陆壳的部分熔融.结合内蒙古东南部蛇绿混杂岩、晚古生代岩浆岩带和沉积环境、三叠纪碰撞相关花岗岩带等研究,推测古亚洲洋东段的闭合发生在晚二叠世;三叠纪进入陆陆碰撞阶段.

       

    • 图  1  研究区地质简图

      Ⅰ.额尔古纳地块;Ⅱ.兴安地块;Ⅲ.松嫩地块;Ⅳ.佳木斯地块;Ⅴ.完达山地体;Ⅵ.华北北缘增生带;Ⅶ.华北板块;F1.蒙古-鄂霍茨克构造带;F2.塔源-喜贵图构造带;F3.贺根山-黑河构造带;F4.嫩江-八里罕构造带;F5.西拉木伦-长春构造带;F6.赤峰-开原断裂;F7.伊通-依兰断裂;F8.敦化-密山断裂;F9.牡丹江断裂.图b据Wu et al.(2011)修改

      Fig.  1.  Geological sketch map of the studied area

      图  2  巴彦查干二云母二长花岗岩的野外宏观(a)及镜下显微(b)照片

      Qtz.石英;Pl.斜长石;Af.碱性长石;Bit.黑云母;Mus.白云母

      Fig.  2.  Photomicrographs of the two-mica monzogranites from Bayanchagan

      图  3  巴彦查干二云母二长花岗岩(D3172-1和1013-1)锆石阴极发光图像

      红色及黄色圆圈分别表示了LA-ICP-MS U-Pb及Hf同位素测试点位置

      Fig.  3.  CL images of zircons for the two-mica monzogranites(D3172-1 and 1013-1)from Bayanchagan

      图  4  巴彦查干二云母二长花岗岩(D3172-1和1013-1)锆石U-Pb谐和图

      Fig.  4.  Zircon U-Pb concordia diagrams for the two-mica monzogranites(D3172-1 and 1013-1)from Bayanchagan

      图  5  巴彦查干三叠纪二云母二长花岗岩的锆石εHf(t)-t图解

      Yang et al.(2006)

      Fig.  5.  Zircon Hf isotopic features for the Triassic two-mica monzogranites from Bayanchagan

      图  6  巴彦查干二云母二长花岗岩SiO2-K2O (a)和A/CNK-A/NK(b)图解

      图a据Peccerillo and Taylor(1976);图b据Maniar and Piccoli(1989)

      Fig.  6.  Plot of SiO2 vs. K2O (a) and A/CNK vs. A/NK (b) for the two-mica monzogranites from Bayanchagan

      图  7  巴彦查干二云母二长花岗岩的球粒陨石标准化稀土元素配分图(a)和原始地幔标准化微量元素蛛网图(b)

      图a标准化值据文献Boynton(1984);图b标准化值据Sun and McDonough(1989)

      Fig.  7.  Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element spider diagrams (b) for the two-mica monzogranites from Bayanchagan

      图  8  巴彦查干二云母二长花岗岩成因类型判别图

      据文献Whalen et al.(1987)

      Fig.  8.  Genetic type discrimination for the two-mica monzogranites from Bayanchagan

      图  9  巴彦查干二云母二长花岗岩源岩判别图解

      A.泥质岩部分熔融;B.杂砂岩部分熔融;C.基性岩源岩部分熔融.据文献Altherr et al.(2000)

      Fig.  9.  Source rock discrimination diagram for the two-mica monzogranites from Bayanchagan

      图  10  巴彦查干二云母二长花岗岩Harker图解

      Fig.  10.  Harker diagrams for the two-mica monzogranites from Bayanchagan

      图  11  巴彦查干二云母二长花岗岩La-La/Sm图解

      据文献Wang et al.(2011)

      Fig.  11.  La-La/Sm diagram for the two-mica monzogranites from Bayanchagan

      图  12  巴彦查干二云母二长花岗岩的R1-R2构造判别图解

      R1=4Si-11(Na+K)-2(Fe+Ti);R2=6Ca+2Mg+Al.①地幔斜长花岗岩;②破坏性活动陆缘(板块碰撞前)花岗岩;③板块碰撞后隆起期花岗岩;④晚造山期花岗岩;⑤非造山区A型花岗岩了;⑥同碰撞(S型)花岗岩;⑦造山期后A型花岗岩.据文献Batchelor (1985)

      Fig.  12.  R1-R2 tectonic discrimination diagram for the two-mica monzogranites from Bayanchagan

      图  13  西拉木伦缝合带蛇绿混杂岩及三叠纪花岗岩时空分布特征

      据沈阳地质调查中心(2019)《大兴安岭地区区域地质调查片区总结与服务产品开发》项目成果图件修改.图中上标a表示中国地质大学(武汉)(2008)1:25万锡林浩特幅区域地质调查报告; 上标b表示中国地质大学(武汉)(2008)1:25万林西县幅区域地质调查报告; 上标c表示内蒙古自治区第十地质矿产勘查开发院(1997)1:5万双井幅地质图

      Fig.  13.  Spatio-temporal distribution features of ophiolitic melange and Triassic granites in Xar Moron suture

      表  1  巴林右旗巴彦查干二云母二长花岗岩主量、稀土元素、微量元素分析结果及特征参数

      Table  1.   Representative major and trace element data of two-mica monzogranites(D3172-1)from Bayanchagan in Balinyouqi

      样品编号 D3172-1 D3172-2 D3172-3 DB18-1-1 DB18-1-4 1013-1
      SiO2 71.20 71.70 72.00 73.17 74.15 74.44
      TiO2 0.165 0.140 0.140 0.247 0.120 0.093
      Al2O3 15.746 15.695 15.393 14.238 13.794 13.401
      Fe2O3 0.771 0.672 0.796 1.572 0.922 0.675
      FeO 0.490 0.580 0.450 0.476 0.373 0.810
      MnO 0.012 0.014 0.015 0.050 0.054 0.025
      MgO 0.372 0.333 0.311 0.172 0.062 0.333
      CaO 1.008 0.915 0.800 0.329 0.494 0.422
      Na2O 3.435 3.619 3.611 3.950 3.145 2.927
      K2O 5.290 5.401 5.219 3.998 5.950 5.983
      P2O5 0.115 0.097 0.103 0.078 0.013 0.068
      LOI 0.914 0.794 0.905 1.263 0.966 0.625
      Total 99.52 99.96 99.74 99.54 100.04 99.80
      Na2O+K2O 8.725 9.020 8.830 7.948 9.095 8.910
      K2O/Na2O 1.540 1.492 1.445 1.012 1.892 2.044
      A/CNK 1.19 1.17 1.18 1.25 1.10 1.11
      A/NK 1.38 1.33 1.33 1.32 1.19 1.19
      Rb 122.62 119.23 118.63 126.21 171.93 184.72
      Ba 1 700.00 1 700.00 1 700.00 709.56 509.85 390.00
      Th 12.593 9.900 12.115 23.415 36.098 11.782
      U 2.502 1.884 1.925 1.547 6.624 6.001
      Ta 0.623 0.600 0.468 3.240 1.291 1.123
      Nb 1.59 1.54 1.17 11.45 6.39 7.27
      Sr 348.48 335.01 310.33 155.04 191.04 142.28
      Zr 136.53 130.87 130.83 158.92 104.83 102.44
      Hf 2.584 2.192 2.228 5.283 4.405 3.397
      Y 5.864 4.898 5.018 9.844 10.348 7.108
      Ni 2.182 1.691 1.362 1.730 3.750 1.515
      Cr 8.710 6.890 6.790 10.380 8.280 6.845
      Ga 17.05 17.30 16.60 20.44 17.35 17.66
      La 41.560 34.574 39.532 31.644 23.743 14.110
      Ce 74.770 61.225 70.689 58.710 42.145 31.540
      Pr 7.732 6.473 7.504 6.406 5.370 3.825
      Nd 25.17 20.88 23.69 21.65 19.55 14.92
      Sm 3.191 2.846 2.945 3.639 4.130 3.587
      Eu 2.300 2.114 2.129 0.599 0.498 0.502
      Gd 3.310 2.757 3.114 2.893 2.995 2.500
      Tb 0.264 0.254 0.265 0.459 0.462 0.384
      Dy 1.039 0.890 0.965 2.011 1.948 1.344
      Ho 0.176 0.148 0.145 0.314 0.313 0.286
      Er 0.478 0.462 0.476 0.809 0.828 0.620
      Tm 0.074 0.061 0.060 0.113 0.123 0.210
      Yb 0.416 0.414 0.381 0.759 0.829 0.718
      Lu 0.064 0.053 0.050 0.101 0.110 0.125
      (La/Yb)N 71.65 59.90 74.43 29.91 20.54 14.10
      δEu 2.16 2.31 2.15 0.56 0.43 0.51
      ∑REE 160.55 133.15 151.95 130.11 103.04 74.67
      LREE/HREE 26.58 25.42 26.85 16.44 12.54 11.07
      10 000Ga/Al 2.05 2.08 2.04 2.71 2.38 2.49
      Rb/Nd 4.87 5.71 5.01 5.83 8.79 12.38
      Rb/Sr 0.35 0.36 0.38 0.81 0.90 1.30
      C/MF 0.70 0.66 0.60 0.19 0.48 0.27
      A/MF 6.01 6.22 6.30 4.57 7.40 4.70
      La/Sm 13.02 12.15 13.42 8.70 5.75 3.93
      锆石饱和温度 784 780 780 797 761 748
      注:主量元素质量分数单位为%;稀土元素和微量元素质量分数单位为10-6;锆石饱和温度单位为℃.
      下载: 导出CSV

      表  2  西拉木伦缝合带蛇绿混杂岩化石及同位素统计

      Table  2.   Fossil and geochronologic data in Xar Moron suture

      序号 位置 化石类型 同位素 资料来源
      岩性 方法 年龄(Ma) 年代
      1 柯单山 薄壳型介形虫 奥陶纪 邵济安等,2017
      2 柯单山 超基性岩 Sm-Nd 665±46 新元古代 陈森煌等,1991
      3 柯单山 辉长岩 U-Pb 281.1±6.4 早二叠世 叶栩松等,2011
      4 柯单山 辉长岩 U-Pb 276 早二叠世 a
      5 五道石门 有孔虫 志留纪-现代 邵济安等,2017
      6 五道石门 小腕足类 寒武-奥陶纪 邵济安等,2017
      7 杏树洼 放射虫 中二叠世 王玉净和樊志勇,1997
      8 杏树洼 辉长岩 U-Pb 273.9±1.3 早二叠世 殷东方,2018
      9 九井子 辉长岩 U-Pb 274.7±1.7 早二叠世 刘建峰等,2016
      10 二八地 牙形石 奥陶-志留纪 邵济安等,2017
      注:a为中国地质大学(武汉)(2008)1:25万林西县幅区域地质调查报告.
      下载: 导出CSV

      表  3  西拉木伦缝合带三叠纪花岗岩同位素年龄统计

      Table  3.   Geochronologic data of Triassic granites in Xar Moron suture

      序号 岩体名称 岩石类型 年龄(Ma) 资料来源
      1 双井子 二云母花岗岩 229.2±4.1 李锦轶等,2007
      2 双井子 二云母二长花岗岩 237.5±2.7 李锦轶等,2007
      3 转山子 花岗岩 245.6±0.9 刘建峰等,2014
      4 转山子 花岗岩 246±2 Wu et al.,2011
      5 建设屯 花岗闪长岩 249±2 刘建峰等,2013
      6 龙头山 花岗岩 241±3 刘伟等,2007
      7 龙头山 花岗岩 226.2±3.9 Liu et al.,2005
      8 新林 花岗闪长岩 241±2 Wu et al.,2011
      9 锡林浩特水库南 花岗岩 233±12 a
      10 白音锡勒牧场 二长花岗岩 246.4±4.7 b
      11 兰家营子 花岗闪长岩 242.1±6.4 a
      12 吴营子 正长花岗岩 249 b
      13 巴彦查干 二云母二长花岗岩 241.7±0.58 本次
      14 巴彦查干 二云母二长花岗岩 232.0±1.9 本次
      注:a表示中国地质大学(武汉)(2008)1:25万锡林浩特市幅区域地质调查报告;b表示内蒙古自治区第十地质矿产勘查开发院(1997)1:5万双井幅地质图.
      下载: 导出CSV
    • Altherr, R., Holl, A., Hegner, E., et al., 2000. High-Potassium, Calc-Alkaline Ⅰ-Type Plutonism in the European Variscides: Northern Vosges (France) and Northern Schwarzwald (Germany). Lithos, 50(1-3): 51-73. https://doi.org/10.1016/s0024-4937(99)00052-3 doi: 10.1016/S0024-4937(99)00052-3
      Atherton, M.P., Ghani, A.A., 2002. Slab Breakoff: A Model for Caledonian, Late Granite Syn-Collisional Magmatism in the Orthotectonic (Metamorphic) Zone of Scotland and Donegal, Ireland. Lithos, 62(3-4): 65-85. https://doi.org/10.1016/s0024-4937(02)00111-1 doi: 10.1016/S0024-4937(02)00111-1
      Bao, Q.Z., Zhang, C.J., Wu, Z.L., et al., 2007. SHRIMP U-Pb Zircon Geochronology of a Carboniferous Quartz-Diorite in Baiyingaole Area, Inner Mongolia and Its Implications.Journal of Jilin University(Earth Science Edition), 37(1):15-23(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb200701003
      Batchelor, R. A., Bowden, P., 1985. Petrogenetic Interpretation of Granitoid Rock Series Using Multicationic Parameters. Chemical Geology, 48(1-4): 43-55. https://doi.org/10.1016/0009-2541(85)90034-8
      Boynton, W.V., 1984. Geochemistry of the Rare Earth Elements: Meteorite Studies. In: Henderson, P., ed., Rare Earth Element Geochemistry. Elsevier, Amsterdam, 63-114. http://d.old.wanfangdata.com.cn/Periodical/dqhx201803005
      Brown, M., Pressley, R.A., 1999.Crustal Melting in Nature: Prosecuting Source Processes.Physics and Chemistry of the Earth, Part A:Solid Earth and Geodesy, 24(3):305-316. https://doi.org/10.1016/s1464-1895(99)00034-4 doi: 10.1016/S1464-1895(99)00034-4
      Bureau of Geology and Mineral Resources of Nei Mongol Autonomous Region, 1991.Regional Geology of Nei Mongol (Inner Mongolia) Autonomous Region. Geological Publishing House, Beijing(in Chinese). http://www.oalib.com/references/17359189
      Chen, S.H., Liu, D.R., Bao, Z.W., et al., 1991.Emplacement Ages and Evolution of Several Ultrabasic Rock Belts on the Northern Margin of the North China Platform.Geochimica, (2): 128-133(in Chinese with English abstract).
      Fan, Z.L., Ke, Y.F., Chen, W., et al., 2012. Age and Its Tectonic Significance of Ⅰ-Type Granite in Xilinhot, Inner Mongolia.Resources Survey & Environment, 33(3):191-197(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HSDZ201203010.htm
      Fang, J.Q., Zhao, P., Xu, B., et al., 2014.Sedimentary Facies Analyses and Discovery of Gastropods from Zhesi Formation in the South of West Ujimqin, Inner Mongolia and Their Significances.Acta Petrologica Sinica, 30(7):1889-1898(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201407005
      Gao, S., Luo, T. C., Zhang, B. R., et al., 1999. Structure and Composition of the Continental Crust in East China. Science in China (Series D), 29(3): 204-213 (in Chinese). doi: 10.1007-BF02878511/
      Healy, B., Collins, W. J., Richards, S. W., 2004. A Hybrid Origin for Lachlan S-Type Granites: The Murrumbidgee Batholith Example. Lithos, 78(1-2): 197-216. https://doi.org/10.1016/j.lithos.2004.04.047
      Hou, K.J., Li, Y.H., Zou, T.R., et al., 2007.Laser Ablation-MC-ICP-MS Technique for Hf Isotope Microanalysis of Zircon and Its Geological Applications.Acta Petrologica Sinica, 23(10):2595-2604(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200710025
      Huang, B.H., Ding, Q.H., 1998.The Angara Flora from Northern China. Acta Geoscientia Sinica, 19(1):97-104(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQXB801.012.htm
      Jahn, B.M., Wu, F.Y., Chen, B., 2000. Massive Granitoid Generation in Central Asia: Nd Isotopic Evidence and Implication for Continental Growth in the Phanerozoic. Episodes, 23: 82-92. doi: 10.18814/epiiugs/2000/v23i2/001
      King, P. L., White, A. J. R., Chappell, B. W., et al., 1997. Characterization and Origin of Aluminous A-Type Granites from the Lachlan Fold Belt, Southeastern Australia. Journal of Petrology, 38(3): 371-391. https://doi.org/10.1093/petroj/38.3.371
      Li, F.L., Qu, X.Y., Liu, L., et al., 2009.Sedimentary Environment on Upper Permian Linxi Group in Inner Mongolia.Acta Sedimentologica Sinica, 27(2):265-272(in Chinese with English abstract).
      Li, J.Y., Gao, L.M., Sun, G.H., et al., 2007.Shuangjingzi Middle Triassic Syn-Collisional Crust-Derived Granite in the East Inner Mongolia and Its Constraint on the Timing of Collision between Siberian and Sino-Korean Paleo-Plates.Acta Petrologica Sinica, 23(3):565-582(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200703004
      Li, W.G., Li, Q.F., Jiang, W.D., 1996.Rock-Stratigraphic Unit in Inner Mongolia.China University of Geosciences Press, Wuhan(in Chinese).
      Liu, W., Siebel, W., Li, X. J., et al., 2005. Petrogenesis of the Linxi Granitoids, Northern Inner Mongolia of China: Constraints on Basaltic Underplating. Chemical Geology, 219(1-4): 5-35. https://doi.org/10.1016/j.chemgeo.2005.01.013
      Liu, Y. S., Hu, Z. C., Gao, S., et al., 2008. In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard. Chemical Geology, 257(1-2): 34-43. https://doi.org/10.1016/j.chemgeo.2008.08.004
      Liu, J.F., Chi, X.G., Zhang, X.Z., et al., 2009.Geochemical Characteristic of Carboniferous Quartz-Diorite in the Southern Xiwuqi Area, Inner Mongolia and Its Tectonic Significance.Acta Geologica Sinica, 83(3):365-376(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200903006
      Liu, J.F., Chi, X.G., Zhao, Z., et al., 2013.Zircon U-Pb Age and Petrogenetic Discussion on Jianshetun Adakite in Balinyouqi, Inner Mongolia.Acta Petrologica Sinica, 29(3):827-839(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201303007
      Liu, J.F., Li, J.Y., Chi, X.G., et al., 2014. Petrological and Geochemical Characteristics of the Early Triassic Granite Belt in Southeastern Inner Mongolia and Its Tectonic Setting. Acta Geologica Sinica, 88(9):1677-1690(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201409005
      Liu, J.F., Li, J.Y., Sun, L.X., et al., 2016.Zircon U-Pb Dating of the Jiujingzi Ophiolite in Bairin Left Banner, Inner Mongolia:Constraints on the Formation and Evolution of the Xar Moron River Suture Zone.Geology in China, 43(6):1947-1962(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI201606008.htm
      Liu, W., Pan, X.F., Xie, L.W., et al., 2007.Sources of Material for the Linxi Granitoids, the Southern Segment of the Da Hinggan Mts.:When and How Continental Crust Grew?.Acta Petrologica Sinica, 23(2):441-460(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200702022
      Liu, Y.J., Li, W.M., Feng, Z.Q., et al., 2017.A Review of the Paleozoic Tectonics in the Eastern Part of Central Asian Orogenic Belt. Gondwana Research, 43:123-148. https://doi.org/10.1016/j.gr.2016.03.013
      Maniar, P. D., Piccoli, P. M., 1989. Tectonic Discrimination of Granitoids. Geological Society of America Bulletin, 101(5): 635-643. https://doi.org/10.1130/0016-7606(1989)101 < 0635:tdog > 2.3.co; 2 doi: 10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2
      Pan, S.Y., Chi, X.G., Sun, W., et al., 2012. Geochemical Characteristics and Tectonic Significance of Late Carboniferous Volcanic Rocks in Benbatu Formation of Sonid Youqi, Inner Mongolia. Global Geology, 31(1):40-50(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sjdz201201005
      Peccerillo, A., Taylor, S.R., 1976. Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area, Northern Turkey. Contributions to Mineralogy and Petrology, 58(1): 63-81. https://doi.org/10.1007/BF00384745
      Ren, S.M., Huang, B.C., 2002.Preliminary Study on Post-Late Paleozoic Kinematics of the Main Blocks of the Paleo-Asian Ocean. Progress in Geophysics, 17(1):113-120(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqwlxjz200201015
      Shang, Q.H., 2004. Discovery and Significance of Permian Radiolarians in Mid-East Neimenggu, North Orogenic Belt. Chinese Science Bulletin, 49(24): 2574-2579(in Chinese). doi: 10.1360/csb2004-49-24-2574
      Shao, J.A., Wang, Y., Tang, K.D., 2017.A Reflection on the Xarmoron Tectonomagmatic Belt, Inner Mongolia, China.Acta Petrologica Sinica, 33(10):3002-3010(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201710002
      Shi, Y.R, Liu, D.Y., Zhang, Q., et al., 2004. SHRIMP Dating of Diorites and Granites in Southern Suzuoqi, Inner Mongolia. Acta Geologica Sinica, 78(6): 789-799(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200406009
      Song, B., Zhang, Y.H., Wan, Y.S., et al., 2002.Mount Making and Procedure of the SHRIMP Dating.Geological Review, 48(Suppl.):26-30(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000005931
      Song, W.W., Zhou, J.B., Guo, X.D., et al., 2012.Geotectonic Setting of Songliao Block:Restriction from Paleozoic Detrital Zircon U-Pb Dating.Global Geology, 31(3):522-535(in Chinese with English abstract). http://cn.bing.com/academic/profile?id=3cef38e647fb4ef7893ed465fa1f12f1&encoded=0&v=paper_preview&mkt=zh-cn
      Sun, S. S., McDonough, W. F., 1989. Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes. Geological Society, London, Special Publications, 42(1): 313-345. https://doi.org/10.1144/gsl.sp.1989.042.01.19 doi: 10.1144/GSL.SP.1989.042.01.19
      Taylor, S.R., McLennan, S.M., 1985. The Continental Crust Its Composition and Evolution. Blackwell Oxford, 1-312.
      Tian, J., Xin, H.T., Teng, X.J., et al., 2019. Tectonic Significance of Carboniferous-Triassic Magmatism in Langshan Area, Inner Mongolia. Earth Science, 44(1): 206-219 (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/dqkx201901015
      Wang, B. Q., Zhou, M. F., Li, J. W., et al., 2011. Late Triassic Porphyritic Intrusions and Associated Volcanic Rocks from the Shangri-La Region, Yidun Terrane, Eastern Tibetan Plateau: Adakitic Magmatism and Porphyry Copper Mineralization.Lithos, 127(1-2): 24-38. https://doi.org/10.1016/j.lithos.2011.07.028
      Wang, C.W., Jin, W., Zhang, X.Z., et al., 2008.New Understanding of the Late Paleozoic Tectonics in Northeastern China and Adjacent Areas.Journal of Stratigraphy, 32(2):119-136(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dcxzz200802001
      Wang, H., Wang, Y.J., Chen, Z.Y., et al., 2005.Discovery of the Permian Radiolarians from the Bayanaobao Area, Inner Mongolia.Journal of Stratigraphy, 29(4):368-371(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dcxzz200504009
      Wang, Q., 1986.Recognition of the Suture between the Sino-Korean and Siberian Paleoplates in the Middle Part of Inner Mongolia. Acta Geologica Sinica, (1):31-43(in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dzxe198601002.htm
      Wang, Y.J., Fan, Z.Y., 1997.Discovery of Permian Radiolarians in Ophiolite Belt on Northern Side of Xarmoron River, Neimonggol and Its Geological Significance. Acta Palaeontologica Sinica, 36(1):58-68(in Chinese with English abstract).
      Whalen, J. B., Currie, K. L., Chappell, B. W., 1987. A-Type Granites: Geochemical Characteristics, Discrimination and Petrogenesis. Contributions to Mineralogy and Petrology, 95(4): 407-419. https://doi.org/10.1007/bf00402202 doi: 10.1007/BF00402202
      Wu, F. Y., Sun, D. Y., Ge, W. C., et al., 2011. Geochronology of the Phanerozoic Granitoids in Northeastern China. Journal of Asian Earth Sciences, 41(1): 1-30. https://doi.org/10.1016/j.jseaes.2010.11.014
      Wu, F.Y., Li, X.H., Yang, J.H., et al., 2007a. Discussions on the Petrogenesis of Granites.Acta Petrologica Sinica, 23(6):1217-1238(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200706001
      Wu, F.Y., Li, X.H., Zheng, Y.F., et al., 2007b. Lu-Hf Isotopic Systematics and Their Applications in Petrology. Acta Petrologica Sinica, 23(2): 185-220 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200702001
      Xiao, W. J., Windley, B. F., Hao, J., et al., 2003. Accretion Leading to Collision and the Permian Solonker Suture, Inner Mongolia, China: Termination of the Central Asian Orogenic Belt. Tectonics, 22(6): 1069. https://doi.org/10.1029/2002tc001484
      Xu, B., Wang, Z.W., Zhang, L.Y., et al., 2018.The Xing-Meng Intracontinent Orogenic Belt.Acta Petrologica Sinica, 34(10):2819-2844(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201810002
      Xu, W.L., Sun, C.Y., Tang, J., et al., 2019.Basement Nature and Tectonic Evolution of the Xing'an-Mongolian Orogenic Belt.Earth Science, 44(5):1620-1646 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx201905017
      Yang, J.H., Wu, F.Y., Shao, J.A., et al., 2006. Constraints on the Timing of Uplift of the Yanshan Fold and Thrust Belt, North China. Earth and Planetary Science Letters, 246(3-4): 336-352. https://doi.org/10.1016/j.epsl.2006.04.029
      Ye, X.S., Liao, Q.N., Ge, M.C., 2011.Petrogenesis and Tectonic Significance of Triassic Peraluminous Granitoids in Xilinhaote and Linxi Area, Inner Mongolia.Geological Science and Technology Information, 30(3):57-64(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb201103007
      Yin, D.F., 2018.The Formation Age, Genesis and Its Geological Significance of the Xingshuwa Tectonic Melange in Inner Mongolia(Dissertation). China University of Geosciences, Beijing(in Chinese with English abstract).
      Yuan, H. L., Gao, S., Liu, X. M., et al., 2004. Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry.Geostandards and Geoanalytical Research, 28(3): 353-370. https://doi.org/10.1111/j.1751-908x.2004.tb00755.x doi: 10.1111/j.1751-908X.2004.tb00755.x
      Yuan, H.L., Wu, F.Y., Gao, S., et al., 2003.Determination of U-Pb Age and Trace Element of Zircon of Cenozoic Intrusion in NE China by Laser-Ablation Inductively Couple Plasma Mass Spectrometry. Chinese Science Bulletin, 4(14):1511-1520(in Chinese).
      Zhang, Q., Jin, W.J., Li, C.D., et al., 2010.On the Classification of Granitic Rocks Based on Whole-Rock Sr and Yb Concentrations Ⅲ:Practice.Acta Petrologica Sinica, 26(12):3431-3455(in Chinese with English abstract). https://www.researchgate.net/publication/285740935_On_the_classification_of_granitic_rocks_based_on_whole-rock_Sr_and_Yb_concentrations_III_Practice
      Zhang, X.F., Zhou, Y., Cao, J., et al., 2018a.Geochronological and Geochemical Features of Bimodal Intrusive Rocks in the Hanwula Area of Xiwu Banner, Inner Mongolia:Constraints on Closure of the Paleo-Asian Ocean.Acta Geologica Sinica, 92(4):665-686(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dizhixb201804003
      Zhang, X.F., Zhou, Y., Liu, J.L., et al., 2018b.Geochronology and Geochemistry for Volcanic Rocks of Dashizhai Formation and its Geological Significance in Xi U Jimqin Banner, Inner Mongolia.Acta Petrologica Sinica, 34(6):1775-1791(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201806014
      Zhao, Y.L., 2010. Late Paleozoic Tectonic Evolution of the Central and Southern Grate Xing'an Ranges: Constrains from Provenance Characteristics of Permian Sandstones(Dissertation). Jilin University, Changchun(in Chinese with English abstract).
      鲍庆中, 张长捷, 吴之理, 等, 2007.内蒙古白音高勒地区石炭纪石英闪长岩SHRIMP锆石U-Pb年代学及其意义.吉林大学学报(地球科学版), 37(1):15-23. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb200701003
      陈森煌, 刘道荣, 包志伟, 等, 1991.华北地台北缘几个超基性岩带的侵位年代及其演化.地球化学, (2):128-133 doi: 10.3321/j.issn:0379-1726.1991.02.004
      范中林, 柯于富, 陈文, 等, 2012.内蒙古锡林浩特I型花岗岩的时代及构造意义.资源调查与环境, 33(3):191-197. doi: 10.3969/j.issn.1671-4814.2012.03.009
      方俊钦, 赵盼, 徐备, 等, 2014.内蒙古西乌珠穆沁旗哲斯组宏体化石新发现和沉积相分析.岩石学报, 30(7):1889-1898. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201407005
      高山, 骆庭川, 张本仁, 等, 1999.中国东部地壳的结构和组成.中国科学(D辑), 29(3):204-213. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd199903002
      侯可军, 李延河, 邹天人, 等, 2007.LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用.岩石学报, 23(10):2595-2604. doi: 10.3969/j.issn.1000-0569.2007.10.025
      黄本宏, 丁秋红, 1998.中国北方安加拉植物群.地球学报, 19(1):97-104. http://www.cnki.com.cn/Article/CJFDTotal-DQXB801.012.htm
      李福来, 曲希玉, 刘立, 等, 2009.内蒙古东北部上二叠统林西组沉积环境.沉积学报, 27(2):265-272. http://d.old.wanfangdata.com.cn/Conference/7587939
      李锦轶, 高立明, 孙桂华, 等, 2007.内蒙古东部双井子中三叠世同碰撞壳源花岗岩的确定及其对西伯利亚与中朝古板块碰撞时限的约束.岩石学报, 23(3):565-582. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200703004
      李文国, 李庆福, 姜万德, 1996.内蒙古自治区岩石地层.武汉:中国地质大学出版社.
      刘建峰, 迟效国, 张兴洲, 等, 2009.内蒙古西乌旗南部石炭纪石英闪长岩地球化学特征及其构造意义.地质学报, 83(3):365-376. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200903006
      刘建峰, 迟效国, 赵芝, 等, 2013.内蒙古巴林右旗建设屯埃达克岩锆石U-Pb年龄及成因讨论.岩石学报, 29(3):827-839. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201303007
      刘建峰, 李锦轶, 孙立新, 等, 2016.内蒙古巴林左旗九井子蛇绿岩锆石U-Pb定年:对西拉木伦河缝合带形成演化的约束.中国地质, 43(6):1947-1962. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi201606008
      刘建峰, 李锦轶, 迟效国, 等, 2014.内蒙古东南部早三叠世花岗岩带岩石地球化学特征及其构造环境.地质学报, 88(9):1677-1690. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201409005
      刘伟, 潘小菲, 谢烈文, 等, 2007.大兴安岭南段林西地区花岗岩类的源岩:地壳生长的时代和方式.岩石学报, 23(2):441-460. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200702022
      内蒙古自治区地质矿产局, 1991.内蒙古自治区区域地质志.北京:地质出版社.
      潘世语, 迟效国, 孙巍, 等, 2012.内蒙古苏尼特右旗晚石炭世本巴图组火山岩地球化学特征及构造意义.世界地质, 31(1):40-50. doi: 10.3969/j.issn.1004-5589.2012.01.005
      任收麦, 黄宝春, 2002.晚古生代以来古亚洲洋构造域主要块体运动学特征初探.地球物理学进展, 17(1):113-120. doi: 10.3969/j.issn.1004-2903.2002.01.015
      尚庆华, 2004.北方造山带内蒙古中、东部地区二叠纪放射虫的发现及意义.科学通报, 49(24):2574-2579. doi: 10.3321/j.issn:0023-074X.2004.24.014
      邵济安, 王友, 唐克东, 2017.有关内蒙古西拉木伦带古生代-早中生代构造环境的讨论.岩石学报, 33(10):3002-3010. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201710002
      石玉若, 刘敦一, 张旗, 等, 2004.内蒙古苏左旗地区闪长-花岗岩类SHRIMP年代学.地质学报, 78(6):789-799. doi: 10.3321/j.issn:0001-5717.2004.06.009
      宋彪, 张玉海, 万渝生, 等, 2002.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论.地质论评, 48(S1):26-30. http://d.old.wanfangdata.com.cn/Periodical/OA000005931
      宋卫卫, 周建波, 郭晓丹, 等, 2012.松辽地块大地构造属性:古生界碎屑锆石年代学的制约.世界地质, 31(3):522-535. doi: 10.3969/j.issn.1004-5589.2012.03.009
      田健, 辛后田, 腾学建, 等, 2019.内蒙古狼山地区石炭纪-三叠纪岩浆作用及其构造意义.地球科学, 44(1):206-219. http://d.old.wanfangdata.com.cn/Periodical/dqkx201901015
      王成文, 金巍, 张兴洲, 等, 2008.东北及邻区晚古生代大地构造属性新认识.地层学杂志, 32(2):119-136. doi: 10.3969/j.issn.0253-4959.2008.02.001
      王惠, 王玉净, 陈志勇, 等, 2005.内蒙古巴彦敖包二叠纪放射虫化石的发现.地层学杂志, 29(4):368-371. doi: 10.3969/j.issn.0253-4959.2005.04.009
      王荃, 1986.内蒙古中部中朝与西伯利亚古板块间缝合线的确定.地质学报, (1):31-43. http://www.cnki.com.cn/Article/CJFDTotal-DZXE198601002.htm
      王玉净, 樊志勇, 1997.内蒙古西拉木伦河北部蛇绿岩带中二叠纪放射虫的发现及其地质意义.古生物学报, 36(1):58-68. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700131556
      吴福元, 李献华, 杨进辉, 等, 2007a.花岗岩成因研究的若干问题.岩石学报, 23(6):1217-1238. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200706001
      吴福元, 李献华, 郑永飞, 等, 2007b. Lu-Hf同位素体系及其岩石学应用.岩石学报, 23(2):185-220. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200702001
      徐备, 王志伟, 张立杨, 等, 2018.兴蒙陆内造山带.岩石学报, 34(10):2819-2844. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201810002
      许文良, 孙晨阳, 唐杰, 等, 2019.兴蒙造山带的基底属性与构造演化过程.地球科学, 44(5):1620-1646. http://d.old.wanfangdata.com.cn/Periodical/dqkx201905017
      叶栩松, 廖群安, 葛梦春, 2011.内蒙古锡林浩特、林西地区三叠纪过铝质花岗岩的成因及构造意义.地质科技情报, 30(3):57-64. doi: 10.3969/j.issn.1000-7849.2011.03.007
      殷东方, 2018.内蒙古杏树洼构造混杂岩形成时代、成因及其地质意义(硕士学位论文).北京: 中国地质大学. http://cdmd.cnki.com.cn/Article/CDMD-11415-1018017741.htm
      袁洪林, 吴福元, 高山, 等, 2003.东北地区新生代侵入体的锆石激光探针U-Pb年龄测定与稀土元素成分分析.科学通报, 48(14):1511-1520. doi: 10.3321/j.issn:0023-074X.2003.14.008
      张旗, 金惟俊, 李承东, 等, 2010.三论花岗岩按照Sr-Yb的分类:应用.岩石学报, 26(12):3431-3455. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201012001
      张晓飞, 周毅, 曹军, 等, 2018a.内蒙古西乌旗罕乌拉地区双峰式侵入体年代学、地球化学特征及其对古亚洲洋闭合时限的制约.地质学报, 92(4):665-686. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201804003
      张晓飞, 周毅, 刘俊来, 等, 2018b.内蒙古西乌旗大石寨组火山岩年代学和地球化学特征及地质意义.岩石学报, 34(6):1775-1791. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201806014
      赵英利, 2010.大兴安岭中南部二叠纪砂岩物源分析对晚古生代区域构造演化的制约(博士学位论文).长春: 吉林大学. http://cdmd.cnki.com.cn/Article/CDMD-10183-2010106963.htm
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    • 收稿日期:  2019-08-28
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