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    内蒙古博克图晶洞花岗岩形成时代、特征及其地质意义

    秦锦华 刘翠 石玉若 罗照华 邓晋福 李玥霄

    秦锦华, 刘翠, 石玉若, 罗照华, 邓晋福, 李玥霄, 2019. 内蒙古博克图晶洞花岗岩形成时代、特征及其地质意义. 地球科学, 44(4): 1295-1310. doi: 10.3799/dqkx.2018.585
    引用本文: 秦锦华, 刘翠, 石玉若, 罗照华, 邓晋福, 李玥霄, 2019. 内蒙古博克图晶洞花岗岩形成时代、特征及其地质意义. 地球科学, 44(4): 1295-1310. doi: 10.3799/dqkx.2018.585
    Qin Jinhua, Liu Cui, Shi Yuruo, Luo Zhaohua, Deng Jinfu, Li Yuexiao, 2019. Formation Age, Characteristics and Geological Significance of Boketu Miarolitic Granite in Inner Mongolia. Earth Science, 44(4): 1295-1310. doi: 10.3799/dqkx.2018.585
    Citation: Qin Jinhua, Liu Cui, Shi Yuruo, Luo Zhaohua, Deng Jinfu, Li Yuexiao, 2019. Formation Age, Characteristics and Geological Significance of Boketu Miarolitic Granite in Inner Mongolia. Earth Science, 44(4): 1295-1310. doi: 10.3799/dqkx.2018.585

    内蒙古博克图晶洞花岗岩形成时代、特征及其地质意义

    doi: 10.3799/dqkx.2018.585
    基金项目: 

    中国地质调查局项目 DD20160056

    中国地质调查局项目 1212011121075

    中国地质调查局项目 12120114020901

    中国地质调查局项目 12120115069701

    详细信息
      作者简介:

      秦锦华(1992-), 男, 博士研究生, 矿物学、岩石学、矿床学专业

      通讯作者:

      刘翠

    • 中图分类号: P581

    Formation Age, Characteristics and Geological Significance of Boketu Miarolitic Granite in Inner Mongolia

    • 摘要: 晶洞花岗岩成因类型和大地构造背景等方面的研究,目前颇具争议.先前的研究认为晶洞碱长、正长花岗岩属于A型花岗岩,形成于伸展环境,近年来的研究发现其成因类型具多样性.报道了博克图晶洞花岗岩的岩石学、岩石地球化学、年代学等方面的特征.SHRIMP锆石U-Pb定年结果为140.8±2.2 Ma,指示其属于早白垩世的产物.且其具有高SiO2,高ALK(Na2O+K2O)(7.99%~8.43%),K2O/Na2O=1.0~1.1,以及低的FeOT(1.15%~1.30%).微量元素富Th、U、Cs、Rb,贫Ba、Sr、P、Ti,10 000*Ga/Al、总稀土含量以及Zr+Nb+Y+Ce值均低于A型花岗岩最低平均值,由此指示其应属于Ⅰ型花岗岩,Hf同位素特征显示其成分为新生地壳来源.动力学机制上,博克图晶洞花岗岩主要受制于早白垩世时期蒙古-鄂霍次克洋闭合作用.在东北地区岩石圈由增厚到减薄转换事件中,早期的新生地壳在地幔物质的底侵作用下发生低程度的部分熔融作用.

       

    • 图  1  东北地区构造简图

      ①蒙古-鄂霍次克缝合带;②德尔布干断裂;③贺根山断裂;④西拉沐沦断裂;⑤嫩江-八里罕断裂;⑥牡丹江断裂;⑦佳木斯-伊通断裂;⑧敦化-密山断裂;⑨锡霍特-阿林中央带断裂;红色五角星为博克图晶洞花岗岩岩体位置.据张兴洲等(2006)修改

      Fig.  1.  Tectonic map of NE China

      图  2  博克图地区地质简图

      据内蒙古区域地质调查院(2007, 内蒙古自治区1:25万扎兰屯幅地质图)改

      Fig.  2.  Geological map of Boketu area

      图  3  博克图晶洞花岗岩野外露头照片

      a.野外露头照片;b.晶洞照片

      Fig.  3.  The field occurrence photos of Boketu miarolitic granite

      图  4  博克图晶洞花岗岩的岩相学照片

      Q.石英;Kf.钾长石;Pl.斜长石;Bi.黑云母;Ms.白云母,Chl.绿泥石

      Fig.  4.  Petrographic photos of Boketu miarolitic granite

      图  5  锆石颗粒的阴极发光图像

      Fig.  5.  Cathodoluminescence images of zircon grains

      图  6  博克图花岗岩锆石SHRIMP U-Pb年龄谐和图

      Fig.  6.  SHRIMP U-Pb concordia diagram of zircon from Boketu miarolitic granite

      图  7  博克图花岗岩的K2O-SiO2图(a)和SiO2-(Na2O+K2O-CaO)图(b)

      A.碱性系列,AC.碱钙性系列,CA.钙碱性系列,A.钙质系列

      Fig.  7.  K2O vs. SiO2 diagram (a) and SiO2 vs. (Na2O+K2O-CaO) diagram (b) of Boketu miarolitic granite

      图  8  博克图花岗岩的微量元素蛛网图(a)和稀土元素配分图(b)

      标准化值据Sun and McDonough(1989)

      Fig.  8.  Primitive mantle-normalized spider diagram(a) and chondrite-normalized REE pattern(b) of Boketu miarolitic granite

      图  9  10 000×Ga/Al-(Zr+Nb+Y+Ce)图解

      Eby(1990)

      Fig.  9.  10 000×Ga/Al-(Zr+Nb+Y+Ce) diagram of Boketu miarolitic granite

      图  10  高分异的Ⅰ型花岗岩、A型花岗岩判别图解

      底图据Collins et al.(1982)

      Fig.  10.  High differentiation (high fractional) Ⅰ-type granite and A-type granite discrimination diagrams

      图  11  岩体SiO2-P2O5图解(a)和Y-Rb图解(b)

      Chappell and White(2001)

      Fig.  11.  SiO2-P2O5 diagram (a) and Y-Rb diagram (b) of Boketu miarolitic granite

      图  12  博克图晶洞花岗岩的锆石εHf(t)-t图解

      Fig.  12.  The zircon εHf(t)-t diagram of Boketu miarolitic granite

      图  13  岩石样品Nb-Y判别图解(a)、Rb-(Yb+Ta)判别图解(b)、Ta-Yb判别图解(c)和A/CNK-A/NK图解(d)

      图a、b、c据Pearce et al.(1984);图d据Maniar and Piccoli(1989).WPG.班内花岗岩,VAG.火山弧花岗岩,ORG.洋中脊花岗岩,syn-COLG.同碰撞花岗岩,IAGIAG.岛弧花岗岩类;CAG.大陆弧花岗岩类;CCG.大陆碰撞花岗岩类;POG.后造山花岗岩类;RRG.与裂谷有关的花岗岩类;OP.大洋斜长花岗岩;CEUG.与大陆的造陆抬升有关的花岗岩类

      Fig.  13.  Nb-Y diagram (a), Rb-(Yb+Ta) diagram (b), Ta-Yb diagram (c) and A/CNK-A/NK diagram(d) of granite samples

      表  1  博克图晶洞花岗岩SHRIMP锆石U-Pb年龄

      Table  1.   The SHRIMP zircon U-Pb ages of Boketu miarolitic granite

      点号 含量(10-6) Th/U 同位素比值 年龄(Ma)
      U Th 206Pb 206Pb/238U ±% 207Pb*/235U ±% 207Pb/206Pb ±% 206Pb/238U 207Pb/235U 207Pb/206Pb
      BKT3-1 263 138 5.23 0.54 0.022 60 2.7 0.161 0 6.0 0.051 6 5.4 144.1±3.9 147.4±3.9 -947±950
      BKT3-2 250 144 4.77 0.60 0.022 21 2.5 0.137 3 6.5 0.046 6 5.7 141.6±3.5 141.3±3.9 28±140
      BKT3-3 148 96 2.67 0.67 0.020 32 4.1 0.119 0 10 0.055 8 7.0 129.7±5.3 131.4±5.6 -1 020±1 900
      BKT3-4 699 446 12.9 0.66 0.021 40 2.2 0.152 3 4.6 0.051 5 4.1 136.5±3.0 137.4±3.3 -5±210
      BKT3-5 590 404 11.5 0.71 0.022 77 2.3 0.152 6 4.9 0.053 7 3.9 145.1±3.4 144.3±3.8 359±88
      BKT3-6 620 386 11.5 0.64 0.021 27 2.4 0.199 6 3.5 0.052 5 3.6 135.7±3.2 140.3±3.5 -462±680
      BKT3-7 115 79 2.20 0.71 0.021 30 3.7 0.149 0 12 0.065 4 8.1 135.9±5.0 139.6±5.4 -1 450±1 800
      BKT3-8 545 323 10.3 0.61 0.021 91 2.1 0.145 8 4.7 0.050 4 4.0 139.7±2.9 139.4±3.3 212±93
      BKT3-9 646 655 12.1 1.05 0.021 78 2.0 0.145 3 4.3 0.050 6 3.6 138.9±2.8 138.5±3.4 225±83
      BKT3-10 422 330 8.57 0.81 0.023 66 2.2 0.195 3 4.5 0.053 9 4.3 150.8±3.3 151.8±3.8 368±97
      BKT3-11 554 337 10.60 0.63 0.021 97 2.4 0.174 2 4.4 0.054 3 3.9 140.1±3.3 142.6±3.7 -234±240
      BKT3-12 345 168 6.62 0.50 0.022 33 2.3 0.146 4 6.0 0.054 5 4.8 142.3±3.3 141.2±3.6 390±110
      BKT3-13 804 475 15.70 0.61 0.022 61 2.2 0.162 9 3.8 0.050 4 3.3 144.1±3.1 145.4±3.4 -52±190
      下载: 导出CSV

      表  2  Hf同位素分析结果

      Table  2.   Hf isotopic analysis results of Boketu miarolitic granite

      样品 176Yb/177Hf 176Lu/177Hf 176Hf/177Hf εHf(0) εHf(t) f(Lu/Hf) TDM1(Ma) TDM2(Ma)
      BKT3-1 0.047 76 0.000 98 0.001 35 0.000 018 0.282 88 0.000 028 3.8 6.87 -0.96 534.09 1 013.46
      BKT3-2 0.047 73 0.000 35 0.001 39 0.000 003 0.282 85 0.000 025 2.8 5.76 -0.96 575.28 1 110.83
      BKT3-3 0.044 42 0.000 34 0.001 28 0.000 004 0.282 81 0.000 021 1.3 4.09 -0.96 632.68 1 254.96
      BKT3-4 0.055 90 0.000 07 0.001 59 0.000 006 0.282 73 0.000 028 -1.6 1.27 -0.95 755.74 1 513.20
      BKT3-5 0.071 01 0.001 78 0.001 96 0.000 042 0.282 75 0.000 031 -0.9 2.08 -0.94 734.64 1 444.60
      BKT3-6 0.062 65 0.000 59 0.001 96 0.000 008 0.282 82 0.000 022 1.7 4.51 -0.94 629.08 1 220.43
      BKT3-7 0.055 08 0.000 29 0.001 64 0.000 019 0.282 82 0.000 024 1.6 4.49 -0.95 627.18 1 223.48
      BKT3-8 0.041 42 0.000 42 0.001 25 0.000 019 0.282 83 0.000 021 2.0 4.92 -0.96 605.04 1 184.99
      BKT3-9 0.047 54 0.000 38 0.001 40 0.000 001 0.282 80 0.000 026 1.0 3.95 -0.96 645.13 1 271.74
      BKT3-10 0.055 34 0.000 71 0.001 60 0.000 015 0.282 83 0.000 024 2.0 5.15 -0.95 608.4 1 170.60
      注:TDM1为单阶段模式年龄;TDM2为两阶段模式年龄;f(Lu/Hf)为分馏因子,Hf同位素数据具体处理参考Wu et al.(2006).
      下载: 导出CSV
    • Bonin, B., 2007.A-Type Granites and Related Rocks:Evolution of a Concept, Problems and Prospects.Lithos, 97(1-2):1-29. https://doi.org/10.1016/j.lithos.2006.12.007
      Chappell, B.W., White, A.J.R., 1974.Two Contrasting Granite Types.Pacific Geology, 8:173-174. http://d.old.wanfangdata.com.cn/NSTLQK/NSTL_QKJJ027419645/
      Chappell, B.W., White, A.J.R., 2001.Two Contrasting Granite Types:25 Years Later.Australian Journal of Earth Sciences, 48(4):489-499. https://doi.org/10.1046/j.1440-0952.2001.00882.x
      Chen, A.X., Zhou, D., Zhang, Q.K., et al., 2018.Age, Geochemistry, and Tectonic Implications of Dulaerqiao Granite, Inner Mongolia.Journal of Earth Science, 29(1):78-92. https://doi.org/10.1007/s12583-017-0817-6
      Chen, C.Y., Gao, Y.F., Wu, H.B., et al., 2016.Zircon U-Pb Chronology of Volcanic Rocks in the Hailaer Basin, NE China and Its Geological Implications.Earth Science, 41(8):1259-1274(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201608002
      Collins, W.J., Beams, S.D., White, A.J.R., et al., 1982.Nature and Origin of A-Type Granites with Particular Reference to Southeastern Australia.Contributions to Mineralogy and Petrology, 80(2):189-200. https://doi.org/10.1007/bf00374895
      Davis, G.A., Zheng, Y.D., Wang, C., et al., 2001.Mesozoic Tectonic Evolution of the Yanshan Fold and Thrust Belt, with Emphasis on Hebei and Liaoning Provinces, Northern China.Memoir of the Geological Society of America, 194(194):171-197. https://doi.org/10.1130/0-8137-1194-0.171
      Deng, J.F., Luo, Z.H., Su, S.G., et al., 2004.Rock Origin, Tectonic Environment and Mineralization.Geological Publishing House, Bejing(in Chinese).
      Deng, J.F., Zhao, H.L., Mo, X.X., et al., 1996.Continent Roots-Plume Tectonic of China—Key to the Continental Dynamics.Geological Publishing House, Beijng (in Chinese).
      Dickinson, W.R., 1971.Plate Tectonics in Geologic History.Science, 174(4005):107-113. https://doi.org/10.1126/science.174.4005.107
      Didier, J., Lameyre, J., 1969.Les Granites du Massif Central Français:Etude Comparée des Leucogranites et Granodiorites.Contributions to Mineralogy and Petrology, 24(3):219-238. https://doi.org/10.1007/bf00376049
      Dong, S.W., Li, T.D., Zhong, D.L., et al., 2009.Recent Progress and Perspective of the Research on J-K East Asian Multi-Direction Convergent Tectonics.Bulletin of National Natural Science Foundation of China, 23(5):281-286(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkxjj200905008
      Eby, G.N., 1990.The A-Type Granitoids:A Review of Their Occurrence and Chemical Characteristics and Speculations on Their Petrogenesis.Lithos, 26(1-2):115-134. https://doi.org/10.1016/0024-4937(90)90043-z
      Hong, D.W., Wang, S.G., Xie, X.L., et al., 2000.Genesis of Positive ε(Nd, t) Granitoids in the Da Hinggan Mts.-Mongolia Orogenic Belt and Growth Continental Crust.Earth Science Frontiers, 7(2):441-456(in Chinese with English abstract).
      Hou, K.J., Li, Y.H., Xie, G.Q., 2007.LA-MC-ICP-MS Technique for Hf Isotope Microanalysis of Zircon.Journal of Chinese Mass Spectrometry Society, 28(Suppl.):26-28 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200710025
      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, J.Y., Guo, F., Li, C.W., et al., 2014.Neodymium Isotopic Variations of Late Paleozoic to Mesozoic Ⅰ- and A-Type Granitoids in NE China:Implications for Tectonic Evolution.Acta Petrologica Sinica, 30(7):1995-2008(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201407013.htm
      Li, J.Y., Zhang, J., Yang, T.N., et al., 2009.Crustal Tectonic Division and Evolution of the Southern Part of the North Asian Orogenic Region and Its Adjacent Areas.Journal of Jilin University(Earth Science Edition), 39(4):584-605(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb200904002
      Li, P.Z., Yu, J.S., 1993.Nianzishan Miarolitic Alkaline Granite Stock, Heilongjiang—Its Ages and Geological Implications.Geochimica, 22(4):389-398(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX199304008.htm
      Lin, Q., Ge, W.C., Wu, F.Y., et al., 2004.Geochemistry of Mesozoic Granites in Da Hinggan Ling Ranges.Acta Petrologica Sinica, 20(3):403-412(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200403004
      Liu, C., Deng, J.F., Xu, L.Q., et al., 2011.A Preliminary Frame of Magma-Tectonic-Mo Metallogenic Events of Mesozoic Era in Da Hinggan Mountains and Xiao Hinggan Mountains Areas.Earth Science Frontiers, 18(3):166-178(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy201103014
      Liu, C.S., Chen, X.M., Chen, P.R., et al., 2003.Subdivision, Discrimination Criteria and Genisis for A Type Rock Suites.Geological Journal of China Universities, 9(4):573-591(in Chinese with English abstract).
      Loiselle, M.C., Wones, D.R., 1979, Characteristics and Origin of Anorogenic Granites.Geol.Soc.Am.Abstr.with Progr., 11, 468.
      Luo, Z.H., Huang, Z.M., Ke, S., 2007.An Overview of Granitoid.Geological Review, 53(S1):180-226(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy-e201803007
      Ma, C.Q., 1989.Magma-Dynamical Conditions on Crystallization Differentiation.Earth Science, 14(3):245-252(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX198903003.htm
      Ma, Y.F., Liu, Y.J., Wen, Q.B., et al., 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(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201712004
      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
      Mo, S.G., Han, M.L., Li, J.Y., 2005.Compositions and Orogenic Processes of Mongolia-Okhotsk Orogen.Journal of Shandong University of Science and Technology (Natural Science), 24(3):50-52, 64(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sdkjdxxb200503014
      Nowell, G.M., Kempton, P.D., Noble, S.R., et al., 1998.High Precision Hf Isotope Measurements of MORB and OIB by Thermal Ionisation Mass Spectrometry:Insights into the Depleted Mantle.Chemical Geology, 149(3-4):211-233. https://doi.org/10.1016/s0009-2541(98)00036-9
      Pearce, J.A., Harris, N.B.W., Tindle, A.G., 1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology, 25(4):956-983. https://doi.org/10.1093/petrology/25.4.956
      Qiu, J.S., Xiao, E., Hu, J., et al., 2008.Petrogenesis of Highly Fractionated Ⅰ-Type Granites in the Coastal Area of Northeastern Fujian Province:Constraints from Zircon U-Pb Geochronology, Geochemistry and Nd-Hf Isotopes.Acta Petrologica Sinica, 24(11):2468-2484(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200811003.htm
      Shao, J.A., 1991.Crust Evolution in the Middle Part of the Northern Margin of Sino-Korean Plate.Peking University Press, Beijing(in Chinese).
      Shao, J.A., Zhang, L.Q., Mu, B.L., et al.2007.Upwelling of Da Hinggan Mountains and Its Geodynamic Background.Geological Publishing House, Beijing, 1-6 (in Chinese).
      She, H.Q., Li, J.W., Xiang, A.P., et al., 2012.U-Pb Ages of the Zircons from Primary Rocks in Middle-Northern Daxinganling and Its Implications to Geotectonic Evolution.Acta Petrologica Sinica, 28(2):571-594(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201202018
      Shi, G.H., Miao, L.C., Zhang, F.Q., et al.2004.Timing and Tectonic Significance of A Type Granite from Xilin Hot, Inner Mongolia.Chinese Science Bulletin, 49(4):384-389 (in Chinese).
      Song, B., Zhang, Y.H., Wan, Y.S., et al., 2002.Mount Making and Procedure of the SHRIMP Dating.Geological Review, 48(S1):26-30(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000005931
      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
      Tong, Y., Hong, D.W., Wang, T., et al., 2010.Spatial and Temporal Distribution of Granitoids in the Middle Segment of the Sino-Mongolian Border and Its Tectonic and Metallogenic Implications.Acta Geoscientica Sinica, 31(3):395-412(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb201003013
      Watson, E.B., Harrison, T.M., 1983.Zircon Saturation Revisited:Temperature and Composition Effects in a Variety of Crustal Magma Types.Earth and Planetary Science Letters, 64(2):295-304. https://doi.org/10.1016/0012-821x(83)90211-x
      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
      Winther, K.T., 1996.An Experimentally Based Model for the Origin of Tonalitic and Trondhjemitic Melts.Chemical Geology, 127(1-3):43-59.https://doi.10.1016/0009-2541(95)00087-9 doi: 10.1016/0009-2541(95)00087-9
      Wu, F.Y., Jahn, B.M., Wilde, S.A., et al.2003.Highly Fractionated Ⅰ-Type Granites in NE China (Ⅰ):Geochronology and Petrogenesis.Lithos, 66(3-4):241-273. https://doi.org/10.1016/S0024-4937(02)00222-0
      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
      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., Sun, D.Y., Li, H.M., et al., 2002.A-Type Granites in Northeastern China:Age and Geochemical Constraints on Their Petrogenesis.Chemical Geology, 187(1-2):143-173. https://doi.org/10.1016/s0009-2541(02)00018-9
      Wu, F.Y., Sun, D.Y., Lin, Q., 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.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98199902003
      Wu, F.Y., Yang, Y.H., Xie, L.W., et al., 2006.Hf Isotopic Compositions of the Standard Zircons and Baddeleyites Used in U-Pb Geochronology.Chemical Geology, 234(1-2):105-126. https://doi.org/10.1016/j.chemgeo.2006.05.003
      Wu, G., Chen, Y.J., Zhao, Z.H., et al., 2009.Geochemistry, Zircon SHRIMP U-Pb Age and Petrogenesis of the East Luoguhe Granites at the Northern End of the Great Hinggan Range.Acta Petrologica Sinica, 25(2):233-247(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200902001
      Xu, M.J., Xu, W.L., Wang, F., et al., 2013.Geochronology and Geochemistry of the Early Jurassic Granitoids in the Central Lesser Xing'an Range, NE China and Its Tectonic Implications.Acta Petrologica Sinica, 29(2):354-368(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201302002
      Xu, W.L., Wang, F., Pei, F.P., et al., 2013.Mesozoic Tectonic Regimes and Regional Ore-Forming Background in NE China:Constraints from Spatial and Temporal Variations of Mesozoic Volcanic Rock Associations.Acta Petrologica Sinica, 29(2):339-353(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201302001
      Zhang, J.H., 2009.Geochronology and Geochemistry of the Mesozoic Volcanic Rocks in the Great Xing'an Range, Northeastern China (Dissertation).China University of Geosciences, Wuhan (in Chinese with English abstract).
      Zhang, K.F., Deng, B., Zhang, F.Q., et al., 2016.Determination of Early Stage of Early Cretaceous Compressive Event in Hailar Basin, NE China, and Its Tectonic Significance.Earth Science, 41(7):1141-1155(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201607006
      Zhang, K.X., Pan, G.T., He, W.H., et al., 2015.New Division of Tectonic-Strata Superregion in China.Earth Science, 40(2):206-233(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx201502004
      Zhang, Q., 2012.Could Granitic Magmas Experience Fractionation and Evolution? Acta Petrologica et Mineralogica, 31(2):252-260(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/yskwxzz201202013
      Zhang, Q., 2013.Is the Mesozoic Magmatism in Eastern China Related to the Westward Subduction of the Pacific Plate? Acta Petrologica et Mineralogica, 32(1):113-128(in Chinese with English abstract).
      Zhang, Q., Wang, Y., Li, C.D., et al., 2006.Granite Classification on the Basis of Sr and Yb Contents and Its Implications.Acta Petrologica Sinica, 22(9):2249-2269(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200609001
      Zhang, X.Z., Yang, B.J., Wu, F.Y., et al., 2006.The Lithosphere Structure in the Hingmong-Jihei (Hinggan-Mongolia-Jilin-Heilongjiang) Region, Northeastern China.Geology in China, 33(4):816-823(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200604011
      Zhang, Z.M., Kang, D.Y., Ding, H.X., et al., 2018.Partial Melting of Himalayan Orogen and Formation Mechanism of Leucogranites.Earth Science, 43(1):82-98(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx201801005
      Zhao, S., Xu, W.L., Tang, J., et al., 2016.Neoproterozoic Magmatic Events and Tectonic Attribution of the Erguna Massif:Constraints from Geochronological, Geochemical and Hf Isotopic Data of Intrusive Rocks.Earth Science, 41(11):1803-1829(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201611001.htm
      Zhao, X.C., Zhou, W.X., Fu, D., et al., 2018.Isotope Chronology and Geochemistry of the Lower Carboniferous Granite in Xilinhot, Inner Mongolia, China.Journal of Earth Science, 29(2):280-294. https://doi.org/10.1007/s12583-017-0942-2
      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.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200004001
      Zonenshain, L.P., Muznin, M.I., Natapov, L.M., 1990.Mongol-Okhotsk Fold Belt.In: Page, B.M., ed., Geology of the USSR: A Plate Tectonic Synthesis.Geophysical Union Gedynamic Series, 21: 97-120.
      Zorin, Y.A., 1999.Geodynamics of the Western Part of the Mongolia-Okhotsk Collisional Belt, Trans-Baikal Region (Russia) and Mongolia.Tectonophysics, 306(1):33-56. https://doi.org/10.1016/s0040-1951(99)00042-6
      陈崇阳, 高有峰, 吴海波, 等, 2016.海拉尔盆地火山岩的锆石U-Pb年龄及其地质意义.地球科学, 41(8):1259-1274. http://earth-science.net/WebPage/Article.aspx?id=3336
      邓晋福, 罗照华, 苏尚国, 等, 2004.岩石成因、构造环境与成矿作用.北京:地质出版社.
      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.
      董树文, 李廷栋, 钟大赉, 等, 2009.侏罗纪/白垩纪之交东亚板块汇聚的研究进展和展望.中国科学基金, 23(5):281-286. doi: 10.3969/j.issn.1000-8217.2009.05.008
      洪大卫, 王式洸, 谢锡林, 等, 2000.兴蒙造山带正ε(Nd, 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
      侯可军, 李延河, 谢桂青, 2007.锆石Hf同位素的LA-MC-ICP-MS分析方法.质谱学报, 28(增刊):26-28. http://d.old.wanfangdata.com.cn/Conference/6529982
      李锦轶, 张进, 杨天南, 等, 2009.北亚造山区南部及其毗邻地区地壳构造分区与构造演化.吉林大学学报(地球科学版), 39(4):584-605. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb200904002
      李竞妍, 郭锋, 李超文, 等, 2014.东北地区晚古生代-中生代Ⅰ型和A型花岗岩Nd同位素变化趋势及其构造意义.岩石学报, 30(7):1995-2008. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201407013
      李培忠, 于津生, 1993.黑龙江碾子山晶洞碱性花岗岩岩体年龄及其意义.地球化学, 22(4):389-398. doi: 10.3321/j.issn:0379-1726.1993.04.009
      林强, 葛文春, 吴福元, 等, 2004.大兴安岭中生代花岗岩类的地球化学.岩石学报, 20(3):403-412. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200403004
      刘昌实, 陈小明, 陈培荣, 等, 2003.A型岩套的分类、判别标志和成因.高校地质学报, 9(4):573-591. doi: 10.3969/j.issn.1006-7493.2003.04.011
      刘翠, 邓晋福, 许立权, 等, 2011.大兴安岭-小兴安岭地区中生代岩浆-构造-钼成矿地质事件序列的初步框架.地学前缘, 18(3):166-178. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201103014
      罗照华, 黄忠敏, 柯珊, 2007.花岗质岩石的基本问题.地质论评, 53(S1):180-226. http://d.old.wanfangdata.com.cn/Conference/7128036
      马昌前, 1989.结晶分异作用的岩浆动力学条件.地球科学, 14(3):245-252. doi: 10.3321/j.issn:1000-2383.1989.03.001
      马永非, 刘永江, 温泉波, 等, 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. http://earth-science.net/WebPage/Article.aspx?id=3707
      莫申国, 韩美莲, 李锦轶, 2005.蒙古-鄂霍茨克造山带的组成及造山过程.山东科技大学学报(自然科学版), 24(3):50-52, 64. doi: 10.3969/j.issn.1672-3767.2005.03.014
      邱检生, 肖娥, 胡建, 等, 2008.福建北东沿海高分异Ⅰ型花岗岩的成因:锆石U-Pb年代学、地球化学和Nd-Hf同位素制约.岩石学报, 24(11):2468-2484. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200811002
      邵济安, 1991.中朝板块北缘中段地壳演化.北京:北京大学出版社.
      邵济安, 张履桥, 牟保磊, 等, 2007.大兴安岭的隆起与地球动力学背景.北京:地质出版社, 1-6.
      佘宏全, 李进文, 向安平, 等, 2012.大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系.岩石学报, 28(2):571-594. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201202018
      施光海, 苗来成, 张福勤, 等, 2004.内蒙古锡林浩特A型花岗岩的时代及区域构造意义.科学通报, 49(4):384-389. doi: 10.3321/j.issn:0023-074X.2004.04.015
      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
      童英, 洪大卫, 王涛, 等, 2010.中蒙边境中段花岗岩时空分布特征及构造和找矿意义.地球学报, 31(3):395-412. http://d.old.wanfangdata.com.cn/Periodical/dqxb201003013
      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
      吴福元, 孙德有, 林强, 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. http://d.old.wanfangdata.com.cn/Periodical/ysxb98199902003
      武广, 陈衍景, 赵振华, 等, 2009.大兴安岭北端洛古河东花岗岩的地球化学、SHRIMP锆石U-Pb年龄和岩石成因.岩石学报, 25(2):233-247. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200902001
      徐美君, 许文良, 王枫, 等, 2013.小兴安岭中部早侏罗世花岗质岩石的年代学与地球化学及其构造意义.岩石学报, 29(2):354-368. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201302002
      许文良, 王枫, 裴福萍, 等, 2013.中国东北中生代构造体制与区域成矿背景:来自中生代火山岩组合时空变化的制约.岩石学报, 29(2):339-353. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201302001
      张吉衡, 2009.大兴安岭中生代火山岩年代学及其地球化学研究(博士学位论文).武汉: 中国地质大学. http://cdmd.cnki.com.cn/Article/CDMD-10491-2009153771.htm
      张科峰, 邓彬, 章凤奇, 等, 2016.海拉尔盆地早白垩世早期挤压变形事件的厘定及其构造意义.地球科学, 41(7):1141-1155. http://earth-science.net/WebPage/Article.aspx?id=3324
      张克信, 潘桂棠, 何卫红, 等, 2015.中国构造-地层大区划分新方案.地球科学, 40(2):206-233. http://earth-science.net/WebPage/Article.aspx?id=3179
      张旗, 2012.花岗质岩浆能够结晶分离和演化吗?岩石矿物学杂志, 31(2):252-260. doi: 10.3969/j.issn.1000-6524.2012.02.013
      张旗, 2013.中国东部中生代岩浆活动与太平洋板块向西俯冲有关吗?岩石矿物学杂志, 32(1):113-128. doi: 10.3969/j.issn.1000-6524.2013.01.010
      张旗, 王焰, 李承东, 等, 2006.花岗岩的Sr-Yb分类及其地质意义.岩石学报, 22(9):2249-2269. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200609001
      张兴洲, 杨宝俊, 吴福元, 等, 2006.中国兴蒙—吉黑地区岩石圈结构基本特征.中国地质, 33(4):816-823. doi: 10.3969/j.issn.1000-3657.2006.04.011
      张泽明, 康东艳, 丁慧霞, 等, 2018.喜马拉雅造山带的部分熔融与淡色花岗岩成因机制.地球科学, 43(1):82-98. http://earth-science.net/WebPage/Article.aspx?id=3726
      赵硕, 许文良, 唐杰, 等, 2016.额尔古纳地块新元古代岩浆作用与微陆块构造属性:来自侵入岩锆石U-Pb年代学、地球化学和Hf同位素的制约.地球科学, 41(11):1803-1829. http://earth-science.net/WebPage/Article.aspx?id=3381
      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
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