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    华北-西伯利亚板块对接带早白垩纪的裂解: 来自西拉木伦断裂带中性岩墙群的锆石U-Pb年龄及地球化学证据

    李益龙 周汉文 钟增球 尹淑苹 李福林

    李益龙, 周汉文, 钟增球, 尹淑苹, 李福林, 2010. 华北-西伯利亚板块对接带早白垩纪的裂解: 来自西拉木伦断裂带中性岩墙群的锆石U-Pb年龄及地球化学证据. 地球科学, 35(6): 921-932. doi: 10.3799/dqkx.2010.107
    引用本文: 李益龙, 周汉文, 钟增球, 尹淑苹, 李福林, 2010. 华北-西伯利亚板块对接带早白垩纪的裂解: 来自西拉木伦断裂带中性岩墙群的锆石U-Pb年龄及地球化学证据. 地球科学, 35(6): 921-932. doi: 10.3799/dqkx.2010.107
    LI Yi-long, ZHOU Han-wen, ZHONG Zeng-qiu, YIN Shu-ping, LI Fu-ling, 2010. Extension of Suture Zone Between North China and Siberia Craton in Early Cretaceous: Insights from Geochronology and Geochemistry of Intermediate Dykes from Xar Moron Fault Belt in Inner Mongolia. Earth Science, 35(6): 921-932. doi: 10.3799/dqkx.2010.107
    Citation: LI Yi-long, ZHOU Han-wen, ZHONG Zeng-qiu, YIN Shu-ping, LI Fu-ling, 2010. Extension of Suture Zone Between North China and Siberia Craton in Early Cretaceous: Insights from Geochronology and Geochemistry of Intermediate Dykes from Xar Moron Fault Belt in Inner Mongolia. Earth Science, 35(6): 921-932. doi: 10.3799/dqkx.2010.107

    华北-西伯利亚板块对接带早白垩纪的裂解: 来自西拉木伦断裂带中性岩墙群的锆石U-Pb年龄及地球化学证据

    doi: 10.3799/dqkx.2010.107
    基金项目: 

    国家重点基础研究"973"项目 2007CB411307

    中国地质调查局项目 1212010510507

    详细信息
      作者简介:

      李益龙(1983-), 男, 博士生, 研究方向为变质岩石学.E-mail: yilong_l@yahoo.com.cn

      通讯作者:

      周汉文, E-mail: hwzhou@cug.edu.cn

    • 中图分类号: P597

    Extension of Suture Zone Between North China and Siberia Craton in Early Cretaceous: Insights from Geochronology and Geochemistry of Intermediate Dykes from Xar Moron Fault Belt in Inner Mongolia

    • 摘要: 在内蒙古林西县西拉木伦断裂带内发育规模较大的中性岩墙群, 岩墙多呈NE3°~5°近直立侵入.对岩石进行了锆石LA-ICP-MS U-Pb定年和详细的岩石地球化学特征研究.锆石LA-ICP-MS U-Pb年龄为132.2±2.2Ma, 岩石侵位于早白垩世.岩石地球化学特征显示岩石具有高钾钙碱性系列-钾玄岩系列的过渡特征, 形成于板内拉张环境, 岩浆源区具有壳幔混源的特征, 是早期俯冲洋壳遭受幔源岩浆底侵作用的结果.岩墙的产状受左旋剪切机制控制, 该机制可能主要与太平洋板块相对亚洲板块的向北运动有关.

       

    • 图  1  研究区构造格局略图

      Fig.  1.  Structure delineation of the research area

      图  2  内蒙古林西县双井地区地质简图

      1.双井片岩;2.花岗质片麻岩;3.志留系西别河组;4.杏树洼蛇绿岩;5.二叠系哲斯组;6.中生代侵入岩;7.中生代火山岩;8.第三系玄武岩;9.第四系;10.断层;11.村庄;12.岩墙采样点

      Fig.  2.  Geological map of Shuangjing area in Linxi County, Inner-Mongolia

      图  3  林西县中性岩墙群单颗粒锆石CL图像(a)和LA-ICP-MS锆石U-Pb谐和图(b)

      圆圈表示剥蚀激光束对应的位置,直径为24μm

      Fig.  3.  Representative CL images (a) and LA-ICP-MS U-Pb concordia diagram (b) of zircons from the intermediate dykes in Linxi County

      图  4  林西县中性岩墙群的分类图解

      a.全碱-SiO2图解(MacDonald and Katsura, 1964);b.AFM图解(Irvine and Baragar, 1971)

      Fig.  4.  Classification of the intermediate dykes in Linxi County

      图  5  林西县中性岩墙群的系列判别

      a.K2O-SiO2图解(Morrison, 1980);b.Th/Yb-Ta/Yb图解(Müller and Groves, 1995)

      Fig.  5.  Rock series Discriminant of the intermediate dykes in Linxi County

      图  6  林西县中性岩墙群微量元素原始地幔标准化蛛网图(a)和稀土元素球粒陨石标准化分布模式(b)

      标准值采用Sun and McDonough (1989)推荐值

      Fig.  6.  Primitive-mantle normalized trace elements distribution patterns (a) and Chondrite normalized REE distribution patterns (b) of the intermediate dykes in Linxi County

      图  7  林西县中性岩墙群的构造背景判别图

      a.FeOt-MgO-Al2O3图解(Pearce et al., 1977);b.TiO2-K2O-P2O5图解(Pearce et al., 1975)

      Fig.  7.  Tectonic discriminant diagrams for intermediate dykes in Linxi County

      表  1  林西县中性岩墙群(8878)的LA-ICP-MS锆石U-Pb分析结果

      Table  1.   LA-ICP-MS zircon U-Pb analytic data for intermediate dykes (8878) in Linxi County

      锆石点号 8878-1 8878-2 8878-3 8878-4 8878-5 8878-6 8878-7 8878-8
      组成 Pb(10-6) 18.45 3.32 2.17 6.22 6.03 6.84 12.55 17.69
      Th(10-6) 364.79 88.04 36.95 185.40 206.70 175.80 386.57 345.24
      U(10-6) 628.84 110.37 73.28 181.22 203.55 215.55 411.52 629.92
      Th/U 0.58 0.80 0.50 1.02 1.02 0.82 0.94 0.55
      含量比值 207Pb/206Pb 0.04945 0.05201 0.05064 0.05181 0.05033 0.05087 0.05216 0.05025
      1σ 0.00099 0.00238 0.00323 0.00431 0.00189 0.00314 0.00237 0.00101
      207Pb/235U 0.14472 0.14615 0.14656 0.14537 0.14199 0.13987 0.14694 0.14606
      1σ 0.00279 0.00652 0.00916 0.01189 0.00520 0.00846 0.00648 0.00284
      206Pb/238U 0.02123 0.02038 0.02099 0.02035 0.02046 0.01994 0.02043 0.02108
      1σ 0.00021 0.00027 0.00033 0.00031 0.00024 0.00025 0.00023 0.00021
      208Pb/232Th 0.00661 0.00665 0.00691 0.00640 0.00620 0.00628 0.00642 0.00668
      1σ 0.00008 0.00013 0.00023 0.00006 0.00010 0.00006 0.00005 0.00008
      年龄(Ma) 207Pb/206Pb 169 286 224 277 210 235 292 207
      1σ 27 78 115 190 63 143 106 27
      207Pb/235U 137 139 139 138 135 133 139 138
      1σ 2 6 8 11 5 8 6 3
      206Pb/238U 135 130 134 130 131 127 130 134
      1σ 1 2 2 2 2 2 1 1
      208Pb/232Th 133 134 139 129 125 127 129 135
      1σ 2 3 5 1 2 1 1 2
      下载: 导出CSV

      表  2  林西县中性岩墙群的主量元素分析结果及处理后数据(%)

      Table  2.   Compositions of major elements and conversion data of the intermediate dykes from Linxi County

      样品 SiO2 Al2O3 Fe2O3 FeO CaO MgO Na2O K2O TiO2 MnO P2O5 H2O+ CO2 Total
      8878-2 52.91 14.91 3.64 3.90 6.31 3.25 2.78 2.77 1.40 0.09 0.48 2.97 4.34 99.75
      8878-3 52.86 15.02 2.68 4.85 6.14 3.41 2.81 3.10 1.43 0.15 0.50 2.95 3.75 99.65
      8878-4 53.27 15.33 2.07 5.40 5.56 3.38 3.79 2.28 1.48 0.11 0.51 2.90 3.55 99.63
      8878-5 54.49 16.72 3.06 3.50 5.53 2.84 3.45 2.88 1.01 0.10 0.42 2.44 2.86 99.30
      8878-6 53.30 15.40 2.52 5.00 5.59 3.42 3.81 2.37 1.50 0.11 0.51 3.05 3.06 99.64
      8878-7 55.33 14.92 3.31 4.10 4.68 3.28 3.78 3.64 1.62 0.09 0.76 2.51 1.68 99.70
       
      换算后
      样品 SiO2 Al2O3 Fe2O3 FeO CaO MgO Na2O K2O TiO2 MnO P2O5 FeOt σ Mg#
      8878-2 57.24 16.13 3.94 4.22 6.83 3.52 3.01 3.00 1.51 0.10 0.52 7.76 2.53 44.67
      8878-3 56.87 16.16 2.88 5.22 6.61 3.67 3.02 3.34 1.54 0.16 0.54 7.81 2.91 45.57
      8878-4 57.17 16.45 2.22 5.80 5.97 3.63 4.07 2.45 1.59 0.12 0.55 7.79 2.99 45.34
      8878-5 57.97 17.79 3.26 3.72 5.88 3.02 3.67 3.06 1.07 0.11 0.45 6.65 3.03 44.74
      8878-6 56.99 16.47 2.69 5.35 5.98 3.66 4.07 2.53 1.60 0.12 0.55 7.77 3.12 45.62
      8878-7 57.93 15.62 3.47 4.29 4.90 3.43 3.96 3.81 1.70 0.09 0.80 7.41 4.04 45.23
      下载: 导出CSV

      表  3  林西县中性岩墙群的微量元素分析结果(10-6)

      Table  3.   Compositions of trace elements of the intermediate dykes in Linxi County

      元素 8878-2 8878-3 8878-4 8878-5 8878-6 8878-7
      Be 1.68 1.95 1.63 1.35 1.64 1.86
      Sc 14.80 15.20 15.00 9.28 15.30 12.70
      V 140.00 144.00 149.00 114.00 152.00 124.00
      Cr 43.30 39.50 31.10 1.87 32.80 63.50
      Co 19.90 20.90 20.60 16.00 21.00 19.90
      Ni 10.60 9.92 9.13 3.51 8.97 27.00
      Cu 29.40 28.40 22.50 15.40 17.60 32.80
      Zn 188.00 200.00 146.00 113.00 130.00 173.00
      Ga 19.70 20.00 20.20 20.70 20.90 22.40
      Rb 92.70 91.50 62.20 75.10 63.40 77.10
      Sr 321 483 646 1048 640 608
      Y 19.2 20.1 20.1 18.1 20.4 24.7
      Zr 226 236 239 174 247 354
      Nb 11.00 11.60 12.20 8.03 12.10 21.60
      Sn 1.72 1.67 1.65 1.24 1.66 2.18
      Cs 4.96 3.58 2.32 2.92 2.55 3.83
      Ba 727 1585 1715 4169 1681 1109
      La 36.1 38.7 35.6 36.1 36.7 59.7
      Ce 72.3 76.8 78.0 67.8 81.8 128
      Pr 9.40 10.1 10.2 8.82 10.4 16.3
      Nd 37.3 40.1 40.1 34.7 41.6 62.0
      Sm 6.98 7.41 7.30 5.89 7.75 10.5
      Eu 1.84 2.17 2.09 1.97 2.14 2.51
      Gd 5.37 5.73 5.70 4.43 5.86 7.37
      Tb 0.73 0.79 0.80 0.60 0.82 1.01
      Dy 3.90 4.13 4.25 3.22 4.25 5.11
      Ho 0.69 0.73 0.72 0.60 0.75 0.90
      Er 1.83 1.90 1.96 1.58 1.95 2.33
      Tm 0.25 0.28 0.27 0.22 0.27 0.32
      Yb 1.46 1.58 1.54 1.39 1.60 1.96
      Lu 0.23 0.25 0.24 0.21 0.25 0.28
      Hf 5.38 5.77 5.73 4.16 5.92 8.15
      Ta 0.65 0.70 1.51 0.50 0.71 1.08
      Pb 196.00 221.00 103.00 73.30 56.80 53.40
      Th 4.51 4.70 4.50 3.34 4.52 3.95
      U 1.25 1.22 1.13 0.85 1.13 1.26
      Eu* 0.88 0.98 0.95 1.13 0.93 0.94
      Ce* 0.94 0.93 0.99 0.90 1.01 1.00
      (La/Yb)n 17.77 17.59 16.63 18.65 16.48 16.31
      (La/Gd)n 5.83 5.86 5.42 7.07 5.42 5.55
      (Dy/Yb)n 1.79 1.75 1.85 1.55 1.78 1.77
      下载: 导出CSV
    • Andersen, T., 2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology, 192(1-2): 59-79. doi: 10.1016/S0009-2541(02)00195-X
      Badarch, G., Cuningham, W.D., Windley, B.F., 2002. A new terrane subdivision for Mongolia: implications for the Phanerozoic crustal growth of Central Asia. Journal of Asian Earth Sciences, 21(1): 87-110. doi:10.1016/ S1367-9120(02)00017-2
      Chen, B., Jahn, B.M., Wilde, S., et al., 2000. Two contrasting Paleozoic magmatic belts in northern Inner Mongolia, China: petrogenesis and tectonic implications. Tectonophysics, 328(1-2): 157-182. doi: 10.1016/S0040-1951(00)00182-7
      Deng, J.F., Su, S.G., Liu, C., et al., 2006. Discussion on the lithospheric thinning of the North China craton: delamination? or thermal erosion and chemical metasomatism?Earth Science Frontiers, 13(2): 105-119 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200602012.htm
      Deng, J.F., Zhao, H.L., Mo, X.X., et al., 1996. Continental roots-plume tectonics of China: key to the continental dynamics. Geological Publishing House, Beijing, 30-39 (in Chinese).
      Fukao, Y., Obayashi, M., Inoue, H., et al., 1992. Subducting slabs stagnant in the mantle transition zone. Journal of Geophysical Research, 97: 4809-4822. doi: 10.1029/91JB02749
      Halls, H.C., 1982. The importance and potential of mafic dyke swarms in studies of geodynamic processes. Geosciences Canada, 9: 145-154. http://www.researchgate.net/publication/285020850_The_importance_and_potential_of_mafic_dyke_swarms_in_studies_of_geodynamic_processes
      Hong, D.W., Wang, S.G., Xie, X.L., et al., 2000. Genesis of positive εNd(t) granitoids in the Da Hinggan MTS-Mongolia oroganic belt and continental crustal growth. Earth Science Frontiers, 7(2): 441-456 (in Chinese with English abstract). http://www.researchgate.net/publication/308357170_Genesis_of_Positive_Ndt_Granitoids_in_the_Da_Hinggan_Mts-Mongolia_Orogenic_Belt_and_Growth_Continental_Crust
      Hu, S.X., Zhao, Y.Y., Hu, Z.H., et al., 1994. Evolution and development of tectonics and magmatism at the active continental margin of the East China (E 106°) during Mesozoic and Cenozoic. Acta Petrologica Sinica, 10(4): 370-381 (in Chinese with English abstract). http://www.researchgate.net/publication/292405644_Evolution_and_development_of_tectonics_and_magmatism_at_the_active_continental_margin_of_east_China_E_106_during_Mesozoic_and_Cenozoic
      Irvine, T.N., Baragar, W.R.A., 1971. A guide to the chemical classification of the common volcanic rocks. Canadian Journal of Earth Sciences, 8: 523-548. doi: 10.1139/e71-055
      Jahn, B.M., Capdevila, R., Liu, D., et al., 2004. Sources of Phanerozoic granitoids in the transect Bayanhongor-Ulaan Baatar, Mongolia: geochemical and Nd isotopic evidence, and implications for Phanerozoic crustal growth. Journal of Asian Earth Sciences, 23(5): 629-653. doi: 10.1016/S1367-9120(03)00125-1
      Khain, E.V., Bibikova, E.V., Kröner, A., et al., 2002. The most ancient ophiolite of the Central Asian fold belt: U-Pb and Pb-Pb zircon ages for the Dunzhugur complex, eastern Sayan, Siberia, and geodynamic implications. Earth and Planetary Science Letters, 199(3-4): 311-325. doi: 10.1016/S0012-821X(02)00587-3
      Khain, E.V., Bibikova, E.V., Salnikova, E.B., et al., 2003. The Palaeo-Asian ocean in the Neoproterozoic and Early Palaeozoic: new geochronologic data and palaeotectonic reconstructions. Precambrian Research, 122(1-4): 329-358. doi: 10.1016/S0301-9268(02)00218-8
      Li, P.W., Gao, R., Guan, Y., et al., 2006. Palaeomagnetie constraints on the final closure time of Solonker-Linxi suture. Journal of Jilin University (Earth Science Edition), 36(5): 744-758 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ200605014.htm
      Li, Y.L., Zhou, H.W., Ge, M.C., et al., 2007. Characteristics and genesis of migmatites within the northern of Shuangjing micro-plate in the West Lamulun fault zone, Inner Mongolia. J. Mineral. Petrol. , 27(4): 22-29 (in Chinese with English abstract). http://www.researchgate.net/publication/289714698_Characteristics_of_genesis_of_migmatites_within_the_northern_Shuangjing_micro-plate_in_the_West_Lamulun_fault_zone_inner-Mongolia_Province
      Li, Y.L., Zhou, H.W., Ge, M.C., et al., 2008. LA-ICP-MS zircon U-Pb dating of migmatite from north of Shuangjing schist in Linxi, Inner Mongolia. J. Mineral. Petrol., 28(2): 10-16 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWYS200802005.htm
      Li, Y.L., Zhou, H.W., Zhong, Z.Q., et al., 2009. Collision processes of North China and Siberian Plates: evidence from LA-ICP-MS zircon U-Pb age on deformed granite in Xar Moron suture zone. Earth Science—Journal of China University of Geosciences, 34(6): 931-938 (in Chinese with English abstract). doi: 10.3799/dqkx.2009.106
      Lu, F.X., Sang, L.K., 2002. Petrology. Geological Publishing House, Beijing, 42-45 (in Chinese).
      Ludwig, K.R., 1991. Isoplot—a plotting and regression program for radiogenic-isotope data. US Geological Survey Open-File Report, 39: 91-445. http://ci.nii.ac.jp/naid/10008802019
      Ma, Z.J., Wang, G.Q., 1999. Strip-shaped tectonic division of contemporary lithospheric structure of eastern China. Geological Journal of China Universities, 5(1): 7-16 (in Chinese with English abstract).
      MacDonald, G.A., Katsura, T., 1964. Chemical composition of Hawaiian lavas. Journal of Petrology, 5(1): 82-133. doi: 10.1093/petrology/5.1.82
      McCulloch, M.T., Gamble, J.A., 1989. Depleted source for volcanic arc basalts: constraints from basalts of Kemadec-Taupo volcanic zone based on trace elements, isotopes and subduction chemical geodynamica. In: Continental magmatism, Inter. Volcanic. Conf. Abstr., New Mexico Bur. Miner. Resour. Bull., 131-180.
      Miao, L.C., Fan, W.M., Liu, D.Y., et al., 2008. Geochronology and geochemistry of the Hegenshan ophiolite complex: implications for late-stage tectonic evolution of the Inner Mongolia-Daxinganling orogenic belt, China. Journal of Asian Earth Sciences, 32(5-6): 348-370. doi: 10.1016/j.jseaes.2007.11.005
      Morrison, G.W., 1980. Characteristics and tectonic setting of shoshonite rock association. Lithos, 13(1): 97-108. doi: 10.1016/0024-4937(80)90067-5
      Müller, D., Groves, D.I., 1995. Potassic igneous rocks and associated gold-copper mineralization. Springer Verlag, Berlin, 1-144.
      Pearce, J.A., Gorman, B.E., Birkett, T.C., 1975. The TiO2-K2O-P2O5 diagram, a method of discrimination between ocean and non-ocean basalts. Earth and Planetary Science Letters, 24: 419-426. doi: 10.1016/0012-821X(75)90149-1
      Pearce, N.J.G., Perkins, W.T., Westgate, J.A., et al., 1997. A compilation of new and published major and trace element data for NIST SRM 610 and NIST SRM 612 glass reference materials. Geostandard and Geoanalytical Research, 21(1): 115-144. doi: 10.1111/j.1751-908X.1997.tb00538.x
      Pearce, T.H., Gorman, B.E., Birkett, T.C., 1977. The relationship between major element chemistry and tectonic enviroment of basic and intermediate volcanic rocks. Earth and Planetary Science Letters, 36(1): 121-132. doi: 10.1016/0012-821X(77)90193-5
      Ren, J.S., Niu, B.G., He, Z.J., et al., 1997. Tectonic framework and geodynamic evolution of eastern China. Geological Research, 29(30): 43-55 (in Chinese with English abstract). http://www.researchgate.net/publication/281665711_Tectonic_frame_and_geodynamic_evolution_of_eastern_China
      Ren, J.S., Wang, Z.X., Chen, B.W., et al., 1999. The tectonics of China from a global view—a guide to the tectonic map of China and adjacent regions. Geological Publishing House, Beijing, 32-33 (in Chinese).
      Sengör, A.M.C., Natal'in, B.A., Burtman, V.S., 1993. Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia. Nature, 364: 299-307. doi: 10.1038/364299a0
      Shang, Q.H., 2004. Occurrences of Permian radiolarians in central and eastern Nei Mongol (Inner Mongolia) and their geological significance to the northern China orogen. Chinese Science Bulletin, 49(24): 2613-2619. doi: 10.1360/04wd0069
      Shao, J.A., Gai, F.Y., Zhang, L.Q., 1998. Coupling of mantle-upwelling and shearing-Mesozoic dyke-swarms in Da-Hinggan mountains, Northeast China. Episodes, 21: 99-103. doi: 10.18814/epiiugs/1998/v21i2/006
      Shao, J.A., Liu, F.T., Chen, H., 2001a. Relationship between Mesozoic magmatism and subduction in Da Hinggan-Yanshan area. Acta Geologica Sinica, 75(1): 56-63 (in Chinese with English abstract).
      Shao, J.A., Zhang, L.Q., 2002. Mesozoic dyke swarms in the north of North China. Acta Petrologica Sinica, 18(3): 312-318 (in Chinese with English abstract). http://www.oalib.com/paper/1473200
      Shao, J.A., Zhang, L.Q., Wei, C.J., et al., 2001b. Composition and features of the Mesozoic bimodal dike swarm in Nankou area, Beijing. Acta Geologica Sinica, 75(2): 205-212 (in Chinese with English abstract). http://www.researchgate.net/publication/287640194_Composition_and_features_of_the_mesozoic_bimodal_dike_swarm_in_Nankou_area_Beijing
      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://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP2002S1006.htm
      Sun, D.Y., Wu, F.Y., Zhang, Y.B., et al., 2004. The final closing time of the west Lamulun River-Changchun-Yanji plate suture zone—evidence from the Dayushan granitic pluton, Jilin Province. Journal of Jilin University (Earth Science Edition), 34(2): 174-181 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ200402003.htm
      Sun, S.S., McDonough, W.F., 1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In: Saundern, A.D., Norry, M.J., eds., Magmatism in the ocean basins. Geological Society of London, Special Publications, 42: 313-345. doi: 10.1144/GSL.SP.1989.042.01.19
      Tang, K.D., 1990. Tectonic development of Paleozoic foldbelts at the north margin of the Sino-Korean craton. Tectonics, 9: 249-260. doi: 10.1029/TC009i002p00249
      The Second Regional Geological Survey Team of Inner Mongolia Autonomous Region, 1997.1: 50000 regional geological surveys report on Shuangjing region (in Chinese).
      Wang, Y.L., Zhang, C.J., Xiu, S.Z., 2001. Th/Hf-Ta/Hf identification of tectonic setting of basalts. Acta Petrologica Sinica, 17(3): 413-421 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200103008.htm
      Wiedenbeck, M., Alle, P., Corfu, F., et al., 1995. Three natural zircon standards for U-Th-Pb, Lu-Hf, trace element and REE analyses. Geostand. Newsl., 19(1): 1-23. doi: 10.1111/j.1751-908X.1995.tb00147.x
      Wu, F.Y., Ge, W.C., Sun, D.Y., et al., 2003. Discussions on the lithospheric thinning in eastern China. Earth Science Frontiers, 10(3): 51-60 (in Chinese with English abstract).
      Wu, F.Y., Sun, D.Y., Lin, Q., et al., 1999. Petrogenesis of the Phanerozoic granites and crustal growth in Northeast China. Acta Petrologica Sinica, 15(2): 181-189 (in Chinese with English abstract). http://www.oalib.com/paper/1471776
      Wu, G.Y., 2002. The Yanshanian orogeny and Late Mesozoic activation in China continent. Chinese Journal of Geology, 37(4): 453-461 (in Chinese with English abstract). http://www.researchgate.net/publication/287849970_The_Yanshanian_orogeny_and_late_Mesozoic_activation_in_the_China_continent
      Wu, L.R., 1985. Mesozoic granitoids in East China. Acta Petrologia Sinica, 1(1): 1-9 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB198501001.htm
      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: 1484-1505. doi: 10.1029/2002TC001484.
      Xu, Y.G., 2001. Thermo-tectonic destruction of the Archaean lithospheric keel beneath the Sino-Korean craton in China: evidence, timing and mechanism. Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy, 26(9-10): 747-757. doi: 10.1016/S1464-1895(01)00124-7
      Xu, Y.G., 2006. Using basalts geochemistry to constrain Mesozoic-Cenozoic evolution of the lithosphere beneath North China Craton. Earth Science Frontiers, 13(2): 93-104 (in Chinese with English abstract). http://kns.cnki.net/KCMS/detail/detail.aspx?dbcode=IPFD&filename=ZGKD200605001027
      Zhai, M.G., Meng, Q.R., Liu, J.M., et al., 2004. Geological features of Mesozoic tectonic regime inversion in eastern North China and implication for geodynamics. Earth Science Frontiers, 11(3): 285-297 (in Chinese with English abstract). http://www.cqvip.com/QK/98600X/20043/10851990.html
      Zhai, M.G., Yang, J.H., Liu, W.J., 2001. Large clusters of gold deposits and large-scale metallogenesis in the Jiaodong Peninsula, eastern China. Science in China (Series D), 44(8): 758-768. doi: 10.1007/BF02907205
      Zhai, M.G., Zhu, R.X., Liu, J.M., et al., 2004. Time range of Mesozoic tectonic regime inversion in eastern North China block. Science in China (Series D), 47(2): 151-159. doi: 10.1360/02ydo416
      Zhang, C.L., Zhou, D.W., Jin, H.L., et al., 1999. Study on the Sr, Nd, Pb and O isotopes of basic dyke swarms in the Wudang block and basic volcanics of the Yaolinghe Group. Acta Petrologica Sinica, 15(3): 430-437 (in Chinese with English abstract).
      Zhang, H.R., 1998. Yanshan event. Acta Goeologica Sinica, 72(2): 103-111 (in Chinese with English abstract).
      Zhang, Y.T., Zhang, L.C., Ying, J.F., et al., 2006. Geochemistry of Zhalantun dyke swarm in North Da Hinggan mountain and its geological implication. Acta Petrologica Sinica, 22(11): 2733-2742 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200611010.htm
      Zhao, D.P., 2004. Global tomographic images of mantle plumes and subducting slabs: insight into deep Earth dynamics. Physics of the Earth and Planetary Interiors, 146(1-2): 3-34. doi: 10.1016/j.pepi.2003.07.032
      Zhao, Y., 1990. The Mesozoic orogenies and tectonic evolution of the Yanshan area. Geological Review, 36(1): 1-13 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP199001000.htm
      Zheng, J.P., O'Reilly, S.Y., Griffin, W.L., et al., 2001. Relict refractory mantle beneath the eastern North China block: significance for lithosphere evolution. Lithos, 57(1): 43-66. doi: 10.1016/S0024-4937(00)00073-6
      Zheng, Y.D., Davis, G.A., Wang, C., et al., 2000. Major Mesozoic tectonic events in the Yanshan belt and the plate tectonic setting. Acta Geologica Sinica, 74(4): 289-302 (in Chinese with English abstract). http://www.researchgate.net/publication/288307824_Major_Mesozoic_tectonic_events_in_the_Yanshan_belt_and_the_plate_tectonic_setting
      Zhou, X.H., 2006. Major transformation of subcontinental lithosphere beneath eastern China in the Cenozoic-Mesozoic: review and prospect. Earth Science Frontiers, 13(2): 50-64 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200602005.htm
      Zhou, X.H., 2009. Major transformation of subcontinental lithosphere beneath North China in Cenozoic-Mesozoic: revisited. Geological Journal of China Universities, 15(1): 1-18 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX200901001.htm
      邓晋福, 苏尚国, 刘翠, 等, 2006. 关于华北克拉通燕山期岩石圈减薄的机制与过程的讨论: 是拆沉, 还是热侵蚀和化学交代?地学前缘, 13(2): 105-119. doi: 10.3321/j.issn:1005-2321.2006.02.009
      邓晋福, 赵海玲, 莫宣学, 等, 1996. 中国大陆根-柱构造: 大陆动力学的钥匙. 北京: 地质出版社, 30-39.
      洪大卫, 王式洸, 谢锡林, 等, 2000. 兴蒙造山带正εNd(t)值花岗岩的成因和大陆地壳生长. 地学前缘, 7(2): 441-456. doi: 10.3321/j.issn:1005-2321.2000.02.012
      胡受奚, 赵乙英, 胡志宏, 等, 1994. 中国东部中-新生代活动大陆边缘构造——岩浆作用演化和发展. 岩石学报, 10(4): 370-381. doi: 10.3321/j.issn:1000-0569.1994.04.003
      李朋武, 高锐, 管烨, 等, 2006. 内蒙古中部索伦-林西缝合带封闭时代的古地磁分析. 吉林大学学报(地球科学版), 36(5): 744-758. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200605014.htm
      李益龙, 周汉文, 葛梦春, 等, 2007. 西拉木伦断裂带双井微地块北缘混合岩的基本特征及其成因机制讨论. 矿物岩石, 27(4): 22-29. doi: 10.3969/j.issn.1001-6872.2007.04.005
      李益龙, 周汉文, 葛梦春, 等, 2008. 内蒙古林西县双井片岩北缘混合岩LA-ICPMS锆石U-Pb年龄. 矿物岩石, 28(2): 10-16. doi: 10.3969/j.issn.1001-6872.2008.02.003
      李益龙, 周汉文, 钟增球, 等, 2009. 华北与西伯利亚板块的对接过程: 来自西拉木伦缝合带变形花岗岩锆石的LA-ICPMS U-Pb年龄证据. 地球科学——中国地质大学学报, 34(6): 931-938. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200906008.htm
      路凤香, 桑隆康, 2002. 岩石学. 北京: 地质出版社, 42-45. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201305002.htm
      马宗晋, 王国权, 1999. 中国大陆东部现今岩石圈结构的板条构造分区. 高校地质学报, 5(1): 7-16. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX901.001.htm
      内蒙古第二区域地质调查队, 1997. 双井地区1: 5万区域地质调查报告.
      任纪舜, 牛宝贵, 和政军, 等, 1997. 中国东部的构造格局和动力学演化. 地学研究, 29(30): 43-55.
      任纪舜, 王作勋, 陈炳蔚, 等, 1999. 从全球看中国大地构造——中国及邻区大地构造图简要说明. 北京: 地质出版社, 32-33.
      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, 刘福田, 陈辉, 等, 2001a. 大兴安岭-燕山晚中生代岩浆活动与俯冲作用关系. 地质学报, 75(1): 56-63. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200101010.htm
      邵济安, 张履桥, 2002. 华北北部中生代岩墙群. 岩石学报, 18(3): 312-318. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200203004.htm
      邵济安, 张履桥, 魏春景, 等, 2001b. 北京南口中生代双峰式岩墙群的组成及其特征. 地质学报, 75(2): 205-212. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200102009.htm
      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(增刊): 26-30. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP2002S1006.htm
      孙德有, 吴福元, 张艳斌, 等, 2004. 西拉木伦河-长春-延吉板块缝合带的最后闭合时间——来自吉林大玉山花岗岩体的证据. 吉林大学学报(地球科学版), 34(2): 174-181. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200402003.htm
      汪云亮, 张成江, 修淑芝, 2001. 玄武岩类形成的大地构造环境的Th/Hf-Ta/Hf图解判别. 岩石学报, 17(3): 413-421. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200103008.htm
      吴福元, 葛文春, 孙德有, 等, 2003. 中国东部岩石圈减薄研究中的几个问题. 地学前缘, 10(3): 51-60. doi: 10.3321/j.issn:1005-2321.2003.03.004
      吴福元, 孙德有, 林强, 等, 1999. 东北地区显生宙花岗岩的成因与地壳增生. 岩石学报, 15(2): 181-189. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB902.003.htm
      吴根耀, 2002. 燕山运动和中国大陆晚中生代的活化. 地质科学, 37(4): 453-461. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200204008.htm
      吴利仁, 1985. 中国东部中生代花岗岩类. 岩石学报, 1(1): 1-9. doi: 10.3321/j.issn:1000-0569.1985.01.002
      徐义刚, 2006. 用玄武岩组成反演中-新生代华北岩石圈的演化. 地学前缘, 13(2): 93-104. doi: 10.3321/j.issn:1005-2321.2006.02.008
      翟明国, 孟庆任, 刘建明, 等, 2004. 华北东部中生代构造体制转折峰期的主要地质效应和形成动力学探讨. 地学前缘, 11(3): 285-297. doi: 10.3321/j.issn:1005-2321.2004.03.027
      翟明国, 杨进辉, 刘文军, 2001. 胶东大型黄金矿集区及大规模成矿作用. 中国科学(D辑), 31(7): 545-552. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200107002.htm
      翟明国, 朱日祥, 刘建明, 等, 2003. 华北东部中生代构造体制转折的关键时限. 中国科学(D辑), 33(10): 913-920. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200310000.htm
      张成立, 周鼎武, 金海龙, 等, 1999. 武当地块基性岩墙群及耀岭河群基性火山岩的Sr、Nd、Pb、O同位素研究. 岩石学报, 15(3): 430-437. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB199903010.htm
      张宏仁, 1998. 燕山事件. 地质学报, 72(2): 103-111. doi: 10.3321/j.issn:0001-5717.1998.02.002
      张玉涛, 张连昌, 英基丰, 等, 2006. 大兴安岭北部扎兰屯脉岩群的地球化学特征及其地质意义. 岩石学报, 22(11): 2733-2742. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200611010.htm
      赵越, 1990. 燕山地区中生代造山运动及构造演化. 地质论评, 36(1): 1-13. doi: 10.3321/j.issn:0371-5736.1990.01.001
      郑亚东, Davis, G.A., 王琮, 等, 2000. 燕山带中生代主要构造事件与板块构造背景问题. 地质学报, 74(4): 289-302. doi: 10.3321/j.issn:0001-5717.2000.04.001
      周新华, 2006. 中国东部中、新生代岩石圈转型与减薄研究若干问题. 地学前缘, 13(2): 50-64. doi: 10.3321/j.issn:1005-2321.2006.02.004
      周新华, 2009. 华北中-新生代大陆岩石圈转型的研究现状与方向——兼评"岩石圈减薄"和"克拉通破坏". 高校地质学报, 15(1): 1-18. doi: 10.3969/j.issn.1006-7493.2009.01.001
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