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大兴安岭绿林林场一带兴华渡口岩群原岩恢复及大地构造环境探讨

贾立民 刘洪章 鞠佳星 李丰

贾立民, 刘洪章, 鞠佳星, 等, 2018. 大兴安岭绿林林场一带兴华渡口岩群原岩恢复及大地构造环境探讨. 地质力学学报, 24 (4): 544-554. DOI: 10.12090/j.issn.1006-6616.2018.24.04.057
引用本文: 贾立民, 刘洪章, 鞠佳星, 等, 2018. 大兴安岭绿林林场一带兴华渡口岩群原岩恢复及大地构造环境探讨. 地质力学学报, 24 (4): 544-554. DOI: 10.12090/j.issn.1006-6616.2018.24.04.057
JIA Limin, LIU Hongzhang, JU Jiaxing, et al., 2018. PROTOLITH RECONSTRUCTION AND GEOTECTONIC ENVIRONMENTAL RESEARCH OF XINGHUADUKOU ROCK GROUP IN LVLIN FORESTRY CENTER, DAXING'ANLING. Journal of Geomechanics, 24 (4): 544-554. DOI: 10.12090/j.issn.1006-6616.2018.24.04.057
Citation: JIA Limin, LIU Hongzhang, JU Jiaxing, et al., 2018. PROTOLITH RECONSTRUCTION AND GEOTECTONIC ENVIRONMENTAL RESEARCH OF XINGHUADUKOU ROCK GROUP IN LVLIN FORESTRY CENTER, DAXING'ANLING. Journal of Geomechanics, 24 (4): 544-554. DOI: 10.12090/j.issn.1006-6616.2018.24.04.057

大兴安岭绿林林场一带兴华渡口岩群原岩恢复及大地构造环境探讨

doi: 10.12090/j.issn.1006-6616.2018.24.04.057
基金项目: 

中国地质调查局地质调查项目 12120115032001

详细信息
    作者简介:

    贾立民(1987-), 男, 硕士, 工程师, 从事地质矿产调查工作。E-mail:790018609@qq.com

  • 中图分类号: P588.3

PROTOLITH RECONSTRUCTION AND GEOTECTONIC ENVIRONMENTAL RESEARCH OF XINGHUADUKOU ROCK GROUP IN LVLIN FORESTRY CENTER, DAXING'ANLING

  • 摘要: 兴华渡口岩群作为额尔古纳地块的基底,其变质年龄、原岩类型及大地构造背景一直是地质学家关注的热点。以大兴安岭北段绿林林场一带兴华渡口岩群作为研究对象,利用锆石U-Pb同位素测年限定了原岩的变质时代,结合岩相学与地球化学综合分析方法开展原岩恢复,并进一步讨论了其形成的大地构造背景。研究认为兴华渡口岩群主要由斜长角闪岩类、浅粒岩类、变粒岩类和石英岩类组成;斜长角闪岩类原岩为基性火山岩,浅粒岩类原岩为英安质凝灰岩,石英岩和变粒岩原岩为泥质粉砂岩;斜长角闪岩类亏损非活动性微量元素Ta、Nd、P,大地构造环境属岛弧环境;浅粒岩类主要亏损Ta、Nd、P、Sr、Ti等元素,形成于大陆边缘造山带环境。绿林林场一带兴华渡口岩群的变质年龄下限为774.1±3.8 Ma。

     

  • 图  1  研究区地质简图

    Figure  1.  Generalized geologic map of the study area

    图  2  细粒斑状含黑云二长花岗岩锆石CL图像特征(白色实线圈为年龄测点位置)

    Figure  2.  CL image features of zircons in fine-grained biotite adamellite (White solid coils are the age measuring positions)

    图  3  细粒斑状含黑云二长花岗岩锆石U-Pb年龄谐和图

    Figure  3.  Concordia plot of zircon U-Pb age in fine-grained biotite adamellite

    图  4  稀土元素/球粒陨石标准化分布形式图

    Figure  4.  standardized distribution pattern of rare earth elements and chondrites

    图  5  微量元素/球粒陨石标准化蛛网图

    Figure  5.  Standardized spider diagram of trace elements and chondrite

    图  6  五大化学类型变质岩和主要造岩矿物在ACF图和A′KF图上的位置[19]

    1—泥质(Al2O3过剩);2—长英质和泥质(K2O过剩);3—钙质;4—基性;5—镁质;Act—阳起石;Andr—钙铁榴石;Jed—铝直闪石;Lm—浊沸石;Lw—硬柱石;Mar—珍珠云母;Mgn—菱镁矿;Opx—斜方辉石;Prh—葡萄石;Prl—叶蜡石;Pu—绿纤石;Pyr—镁铝榴石;Sca—方柱石;Ves—符山石;Zo—黝帘石;Ms—白云母;Bi—黑云母; Cc—方解石;Wo—硅灰石;Dol—白云石;Di—透辉石;Tr—透闪石;Ser—绢云母;Tc—滑石;Ant—直闪石;Cum—镁铁闪石;Brc—水镁石;Alm—铁铝榴石;Ch—绿泥石;Cld—硬绿泥石;Crd—堇青石;St—十字石;Als—Al2SiO5矿物;An—钙长石;Stp—黑硬绿泥石;Kf—钾长石;Ep—绿帘石;Gro—钙铝榴石

    Figure  6.  Positions of five major metamorphic rocks of chemical types and the main rock-forming minerals in Pictures ACF and A′KF[19]

    图  7  周世泰的K-A图解[20]

    A—火成岩区;B—沉积岩区;B1—泥质粉砂岩区;B2—碳酸盐亚区

    Figure  7.  Zhou Shitai K-A diagram[20]

    图  8  变质岩的Mg-K图解[21]

    Ⅰ—细碧岩-角斑岩区;Ⅱ—白云泥灰岩区;Ⅲ—粘土岩区;Ⅳ—富钾火山岩区;Ⅴ—未定区;Ⅵ—玄武岩区;Ⅶ—英安质凝灰岩区

    Figure  8.  Mg-K diagram of metamorphic rocks[21]

    图  9  F3—F2图解[21]

    OFB—大洋底玄武岩;LKT—岛弧拉斑玄武岩;CAB—钙碱质玄武岩;SHO—钾玄岩

    Figure  9.  F3-F2 diagrams[21]

    图  10  里特曼—戈蒂里图解[21]

    A—非造山带火山岩;B—造山带火山岩;C—A、B区派生的碱性、偏碱性火山岩

    Figure  10.  Rittman-Dagger diagram[21]

    表  1  细粒斑状含黑云二长花岗岩锆石LA-ICP-MS分析结果

    Table  1.   The zircon LA-ICP-MS analysis results of fine-grained biotite adamellite

    测点 Pb U 206Pb/238U 207Pb/235U 207Pb/206Pb (206Pb/238U)/
    Ma
    (207Pb/235U)/
    Ma
    (207Pb/206Pb)/
    Ma
    /×10-6
    1 98 673 0.1276 1.1506 0.0654 774.03 777.51 787.04
    2 41 276 0.1271 1.1679 0.0668 771.47 785.67 831.48
    3 139 1283 0.0964 0.8602 0.0646 593.04 630.24 761.12
    4 54 364 0.1269 1.1380 0.0648 770.24 771.54 768.52
    5 63 422 0.1278 1.1787 0.0669 775.42 790.71 835.18
    6 68 449 0.1274 1.1852 0.0674 772.79 793.71 851.54
    7 82 544 0.1286 1.1468 0.0647 779.80 775.73 764.82
    8 138 1146 0.1038 0.9648 0.0675 636.53 685.78 853.70
    9 99 668 0.1274 1.1638 0.0662 773.04 783.72 812.96
    10 78 553 0.1286 1.1988 0.0676 779.75 800.03 857.40
    11 94 593 0.1272 1.1714 0.0668 771.70 787.29 831.48
    12 81 542 0.1266 1.1461 0.0657 768.39 775.38 795.99
    13 104 697 0.1154 1.0192 0.0641 704.18 713.53 744.14
    14 49 368 0.1157 1.0979 0.0687 705.78 752.31 888.58
    15 74 473 0.1358 1.3157 0.0697 820.66 852.63 920.37
    16 86 538 0.1387 1.2450 0.0653 837.12 821.15 783.34
    17 129 1201 0.0976 0.8581 0.0638 600.29 629.11 744.45
    18 62 407 0.1270 1.2126 0.0691 771.01 806.39 901.85
    19 77 499 0.1277 1.1784 0.0667 774.70 790.56 827.78
    20 70 469 0.1280 1.2004 0.0677 776.73 800.76 861.11
    21 181 1409 0.1127 1.0357 0.0662 688.14 721.77 812.96
    22 131 1040 0.1131 1.0353 0.0660 690.93 721.60 805.56
    23 92 614 0.1280 1.1972 0.0675 776.63 799.31 853.70
    24 53 352 0.1282 1.1511 0.0650 777.60 777.74 772.23
    下载: 导出CSV

    表  2  兴华渡口岩群岩石主量元素特征数据表

    Table  2.   Characteristic data table of major elements in rocks of Xinghuadukou Rock group

    序号 时代 岩性 样号 氧化物含量/%
    SiO2 TiO2 Al2O3 Fe2O3 FeO MnO MgO CaO Na2O K2O P2O5 烧失量
    1 中元古代 斜长角闪岩 PM13YQ5 51.72 1.01 10.51 1.47 7.08 0.14 12.97 8.47 2.39 1.14 0.18 2.69 99.79
    2 石英岩 PM13YQ6 93.46 0.09 1.30 2.88 0.87 0.11 0.11 0.06 0.03 0.29 0.023 0.77 99.99
    3 黑云石英岩 PM13YQ9 87.32 0.30 4.61 2.03 1.88 0.036 0.87 0.08 0.14 0.80 0.045 1.85 99.96
    4 二长浅粒岩 PM06YQ1 64.74 0.70 17.36 1.68 1.12 0.091 0.66 1.24 5.27 6.23 0.18 0.55 99.82
    5 二长浅粒岩 PM06YQ2 72.84 0.29 13.71 1.27 1.42 0.048 0.27 0.91 3.56 4.03 0.15 1.20 99.70
    6 二长浅粒岩 PM06YQ6 72.13 0.32 13.38 1.08 2.12 0.086 0.49 0.71 2.97 5.15 0.10 1.12 99.66
    均值 69.90 0.44 14.82 1.35 1.55 0.070 0.47 0.95 3.93 5.14 0.14 0.96 99.73
    7 黑云斜长变粒岩 PM06YQ4 68.39 1.22 15.33 0.98 4.05 0.089 1.63 0.53 0.55 4.50 0.086 2.48 99.84
    8 变粒岩 PM06YQ5 60.97 0.97 20.73 1.95 4.75 0.062 1.21 0.11 0.29 4.68 0.11 4.01 99.84
    9 变粒岩 PM13YQ7 60.85 1.05 17.82 1.37 4.83 0.10 2.53 3.19 3.09 2.86 0.17 1.87 99.74
    均值 63.40 1.08 17.96 1.44 4.54 0.08 1.79 1.27 1.31 4.02 0.12 2.79 99.81
    下载: 导出CSV

    表  3  研究区兴华渡口岩群稀土元素含量及特征参数表

    Table  3.   The content of rare earth elements and the characteristic parameters of Xinghuadukou Rock group in the study area

    序号 样号 稀土元素含量/×10-6 特征参数值
    La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Y ΣREE LREE HREE LR/HR δEu δCe (La/Yb)N (Ce/Yb)N (Sm/Eu)N
    1 PM13YQ5 24.3 45.6 6.31 26.0 4.99 1.51 3.91 0.59 3.13 0.53 1.48 0.21 1.28 0.20 14.4 134.37 108.63 11.33 9.59 1.01 0.87 12.82 9.24 1.25
    基性(维) 27 4.5 4 20 5 1 5 0.8 1 2 0.2 2 0.6 20
    2 PM13YQ6 9.23 23.0 2.38 9.59 1.77 0.29 1.46 0.23 1.28 0.23 0.66 0.10 0.63 0.10 5.64 56.61 46.3 4.68 9.9 0.54 1.16 9.92 9.51 2.28
    3 PM13YQ9 15.0 28.4 3.42 12.9 2.66 0.46 2.41 0.41 2.47 0.44 1.22 0.19 1.20 0.19 11.9 83.23 62.86 8.52 7.38 0.55 0.92 8.46 6.13 2.18
    4 PM06YQ1 84.2 163 18.9 70.0 10.1 2.05 8.61 1.04 4.55 0.80 2.27 0.31 2.01 0.34 22.4 390.27 347.93 19.93 17.46 0.66 0.94 28.26 20.95 1.86
    5 PM06YQ2 44.3 90.3 8.32 32.7 6.43 2.06 6.13 1.08 6.85 1.43 4.15 0.71 4.61 0.75 40.6 250.47 184.1 25.72 7.16 0.99 1.06 6.47 5.07 1.18
    6 PM06YQ6 75.2 137 17.4 70.4 13.3 3.04 12.1 1.97 11.0 2.21 6.20 0.95 5.78 0.97 50.8 408.12 316.13 41.18 7.68 0.72 0.88 8.77 6.12 1.64
    均值 67.9 129. 14.9 57.7 9.9 2.4 9.0 1.4 7.5 1.5 4.2 0.7 4.1 0.7 38.0 349.62 282.72 28.94 10.77 0.79 0.96 14.50 10.71 1.56
    酸性(维) 60 100 12 46 9 1.5 9 2.5 2 4 0.3 4 1 34
    7 PM06YQ4 50.4 103 12.4 48.6 8.91 1.13 7.77 1.20 6.37 1.21 3.26 0.48 3.00 0.50 35.3 283.91 224.79 23.78 9.45 0.41 0.97 11.31 8.91 2.98
    8 PM06YQ5 64.2 130 15.6 60.3 10.9 1.60 9.05 1.36 6.57 1.17 3.14 0.46 2.83 0.46 31.8 339.88 283.07 25.03 11.31 0.48 0.96 15.28 11.91 2.58
    9 PM13YQ7 40.0 83.3 10.7 39.3 6.48 1.90 5.14 0.71 3.59 0.63 1.83 0.27 1.75 0.29 16.7 212.54 181.64 14.21 12.78 0.98 0.95 15.42 12.33 1.28
    均值 51.5 105 12.9 49.4 8.78 1.54 7.32 1.09 5.51 1.00 2.74 0.40 2.53 0.42 27.9 278.78 229.83 21.01 11.18 0.62 0.96 14.00 11.05 2.28
    页岩+粘土岩(维) 40 50 5 23 6.5 1 6.5 0.9 1 2.5 0.25 3 0.7 30
    下载: 导出CSV

    表  4  研究区兴华渡口岩群微量元素含量及特征参数表

    Table  4.   The content of trace elements and characteristic parameters of Xinghuadukou Rock group in the study area

    序号 样号 微量元素含量/×10-6 特征参数值
    Ba Rb Th K Nb Ta Sr Zr Hf Ti Cr Co Ni V U Rb/Sr Zr/Hf K/Rb Nb/Ta
    1 PM13YQ5 495 32.5 4.03 9481 6.75 0.42 500 114 3.76 6034 500 53.2 159 164 0.78 0.07 30.5 290 15.7
    基性(维) 300 45 3 8300 20 0.48 440 100 1 9000 200 45 160 200 0.5 0.10 100 184 41.7
    2 PM13YQ6 30.5 13.9 1.42 2377 1.98 0.14 6.99 29.7 0.881 541 18.9 7.69 9.89 9.80 0.75 1.99 338 170 13.8
    3 PM13YQ9 117 31.7 4.58 6619 7.54 0.49 10.9 114 3.78 1775 30.9 9.50 21.8 19.8 1.38 2.91 30.3 208 15.1
    4 PM06YQ1 677 102 8.84 51720 16.9 0.87 125 569 12.2 4203 3.33 1.59 1.81 24.5 1.68 0.82 46.6 505 19.3
    5 PM06YQ2 1693 120 13.1 33493 20.1 1.30 149 428 12.1 1754 5.78 1.15 1.98 8.18 3.23 0.80 35.3 278 15.4
    6 PM06YQ6 1974 132 17.9 42781 18.2 1.17 148 452 12.2 1936 6.42 1.65 1.03 14.0 3.27 0.89 37.0 322 15.5
    均值 14488 118 13.3 42664 18.4 1.12 141 483 12.2 2631 5.18 1.46 1.61 15.6 2.73 0.84 39.6 360 16.5
    酸性(维) 830 200 18 33400 20 3.5 300 200 1 2300 25 5 8 40 3.5 0.67 200 167 5.71
    7 PM06YQ4 547 214 17.2 37372 24.6 1.52 42.9 356 10.6 7316 94.1 18.2 33.1 137 1.84 5.01 33.4 173 16.2
    8 PM06YQ5 806 200 23.1 38868 19.6 1.39 49.6 233 7.31 5840 90.0 6.10 28.9 129 3.56 4.04 31.9 193 14.1
    9 PM13YQ7 1177 93.8 11.8 23755 15.8 0.72 567 226 6.36 6303 65.6 17.4 23.0 118 1.33 0.17 35.4 253 21.7
    均值 843 169 17.3 33331 20.0 1.21 219 272 8.11 6486 83.2 13.9 28.33 128 2.25 0.77 33.5 196 16.5
    页岩+粘土岩(维) 800 200 11 22800 20 3.5 450 200 6 4500 100 20 95 130 3.2 0.44 33.3 114 5.71
    下载: 导出CSV
  • [1] 表尚虎, 李仰春, 何晓华, 等.黑龙江省塔河绿林林场一带兴华渡口群岩石地球化学特征[J].中国区域地质, 1999, 18(1):28~33. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zqyd901.004&dbname=CJFD&dbcode=CJFQ

    BIAO Shanghu, LI Yangchun, HE Xiaohua, et al. The geochemical characteristics of the Xinghuadukou group in the Lülin forestry center, Tahe, Heilongjiang Province[J]. Regional Geology of China, 1999, 18(1):28~33. (in Chinese with English abstract) http://kns.cnki.net/KCMS/detail/detail.aspx?filename=zqyd901.004&dbname=CJFD&dbcode=CJFQ
    [2] 孙广瑞, 李仰春, 张昱.额尔古纳地块基底地质构造[J].地质与资源, 2002, 11(3):129~139. http://manu39.magtech.com.cn/Geophy/CN/article/downloadArticleFile.do?attachType=PDF&id=13452

    SUN Guangrui, LI Yangchun, ZHANG Yu. The basement tectonics of Ergun massif[J]. Geology and Resources, 2002, 11(3):129~139. (in Chinese with English abstract) http://manu39.magtech.com.cn/Geophy/CN/article/downloadArticleFile.do?attachType=PDF&id=13452
    [3] 葛文春, 隋振民, 吴福元, 等.大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及地质意义[J].岩石学报, 2007, 23(2):423~440. http://www.oalib.com/paper/1473070

    GE Wenchun, SUI Zhenmin, WU fuyuan, et al. Zircon U-Pb ages, Hf isotopic characteristics and their implications of the early Paleozoic granites in the northeastern Da Hinggan Mts., northeastern China[J]. Acta Petrologica Sinica, 2007, 23(2):423~440. (in Chinese with English abstract) http://www.oalib.com/paper/1473070
    [4] 武广. 大兴安岭北部区域成矿背景与有色、贵金属矿床成矿作用[D]. 长春: 吉林大学, 2006, 31~36. http://cdmd.cnki.com.cn/Article/CDMD-10183-2006094308.htm

    WU Guang. Metallogenic setting and metallogenesis of nonferrous-precious metals in northern Da Hinggan Moutain[D]. Changchun: Jilin University, 2006, 31~36. (in Chinese with English abstract) http://cdmd.cnki.com.cn/Article/CDMD-10183-2006094308.htm
    [5] 表尚虎, 赵海滨, 傅俊彧.黑龙江黑河变质地层微古植物化石的发现[J].中国区域地质, 2000, 19(4):445~447. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200004018

    BIAO Shanghu, ZHAO Haibin, FU Junyu. Discovery of microflora fossils in metamorphic strata at Heihe, Heilongjiang[J]. Regional Geology of China, 2000, 19(4):445~447. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200004018
    [6] 赵硕, 许文良, 王枫, 等.额尔古纳地块新元古代岩浆作用:锆石U-Pb年代学证据[J].大地构造与成矿学, 2016, 40(3):573~587. http://mall.cnki.net/magazine/Article/ZQYD2013Z1012.htm

    ZHAO Shuo, XU Wenliang, WANG Feng, et al. Neoproterozoic magmatisms in the Erguna massif, NE China:Evidence from Zircon U-Pb geochronology[J]. Geotectonica et Metallogenia, 2016, 40(3):573~587. (in Chinese with English abstract) http://mall.cnki.net/magazine/Article/ZQYD2013Z1012.htm
    [7] 表尚虎, 郑卫政, 周兴福.大兴安岭北部锆石U-Pb年龄对额尔古纳地块构造归属的制约[J].地质学报, 2012, 86(8):1262~1272. http://www.cqvip.com/QK/95080X/201208/43758846.html

    BIAO Shanghu, ZHENG Weizheng, ZHOU Xingfu. Zircon U-Pb age of the north Da Hinggan Mts., NE China and its constraint to attribute of the Ergun block[J]. Acta Geologica Sinica, 2012, 86(8):1262~1272. (in Chinese with English abstract) http://www.cqvip.com/QK/95080X/201208/43758846.html
    [8] 李仰春, 周兴福, 李永秀, 等.大兴安岭北段兴华渡口岩群多期褶皱解析及变质变形关系[J].前寒武纪研究进展, 2000, 23(1):44~45. https://www.wenkuxiazai.com/word/3f436c00de80d4d8d15a4f13-1.doc

    LI Yangchun, ZHOU Xingfu, LI Yongxiu, et al. The relation ship between the Metamorphism and Deformation of Xinghuadukou Rock group in north part Daxiang'anling[J]. Progress in Precambrian Research, 2000, 23(1):44~45. (in Chinese with English abstract) https://www.wenkuxiazai.com/word/3f436c00de80d4d8d15a4f13-1.doc
    [9] 苗来成, 刘敦一, 张福勤, 等.大兴安岭韩家园子和新林地区兴华渡口群和扎兰屯群锆石SHRIMP U-Pb年龄[J].科学通报, 2007, 52(5):591~601. http://www.cqvip.com/QK/94252X/2007005/24047083.html

    MIAO Laicheng, LIU Dunyi, ZHANG Fuqin, et al. Zircon SHRIMP U-Pb ages of the "Xinghuadukou Group" in Hanjiayuanzi and Xinlin areas and the "Zhalantun Group" in Inner Mongolia, Da Hinggan Mountains[J]. Chinese Science Bulletin, 2007, 52(8):1112~1124. http://www.cqvip.com/QK/94252X/2007005/24047083.html
    [10] 葛文春, 吴福元, 周长勇, 等.大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约[J].科学通报, 2005, 50(12):1239~1247. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kxtb200512014&dbname=CJFD&dbcode=CJFQ

    GE Wenchun, WU Fuyuan, ZHOU Changyong, et al. Emplacement age of the Tahe granite and its constraints on the tectonic nature of the Ergun block in the northern part of the Da Hinggan Range[J]. Chinese Science Bulletin, 2005, 50(18):2097~2105. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kxtb200512014&dbname=CJFD&dbcode=CJFQ
    [11] 赵超. 十六站幅N51E0240231/5区域地质调查报告[R]. 黑龙江地质调查总院, 2010.

    ZHAO Chao. 1: 50000 regional geological survey report in Shiliuzhan[R]. General Institute of Geological Survey of Heilongjiang, 2010. (in Chinese)
    [12] 孙广瑞, 李庆业, 张天柱, 等. 东方红林场幅N-51-(34) 1/20万区域地质调查报告[R]. 黑龙江地矿局第二区调大队, 1989.

    SUN Guangrui, LI Qingye, ZHANG Tianzhu, et al. 1: 200000 regional geological survey report in Dongfanghonglinchang[R]. Heilongjiang Geological and Mining Bureau Second Zone Adjustment Brigade, 1989. (in Chinese)
    [13] 周兴福, 李仰春, 杨晓平, 等. 呼中镇幅N51C0040031/25万区域地质调查报告[R]. 黑龙江省地质调查总院齐齐哈尔分院第四地质队, 2000.

    ZHOU Xingfu, LI Yangchun, YANG Xiaoping, et al. 1: 250000 regional geological survey report in Huzhongzhen[R]. The Fourth Geological Team of Qigihar Branch of Heilongjiang General Survey Institute of Geology, 2000. (in Chinese)
    [14] 王洪波, 杨晓平.大兴安岭北段新一轮国土资源大调查以来的主要基础地质成果与进展[J].地质通报, 2013, 32(2~3):525~532. https://www.wenkuxiazai.com/doc/8793cf0a312b3169a451a49e.html

    WANG Hongbo, YANG Xiaoping. Main geological achievements and progress of the new round of national land and resources survey in north Daxinganling[J]. Geological Bulletin of China, 2013, 32(2~3):525~532. (in Chinese with English abstract) https://www.wenkuxiazai.com/doc/8793cf0a312b3169a451a49e.html
    [15] 潘桂堂, 肖庆辉.中国大地构造图(1:2500000)[M].北京:地质出版社, 2015, 36~37.

    PAN Guitang, XIAO Qinghui. Explanatory note to the tectonic map of China[M]. Beijing:Geological Publishing House, 2015, 36~37. (in Chinese)
    [16] 李怀坤, 耿建珍, 郝爽, 等.用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究[J].矿物学报, 2009, 29(S1):600~601. http://www.cnki.com.cn/Article/CJFDTotal-XBDZ198604016.htm

    LI Huaikun, GENG Jianzhen, HAO Shuang, et al. Laser ablation multiple receiver plasma mass spectrometer(LA-MC-ICP-MS)determination of the isotope age of U-Pb in Zircon[J]. Acta Mineralogica Sinica, 2009, 29(S1):600~601. (in Chinese) http://www.cnki.com.cn/Article/CJFDTotal-XBDZ198604016.htm
    [17] Nasdala L, Hofmeister W, Norberg N, et al. Zircon M257-A homogeneous natural reference material for the ion microprobe U-Pb analysis of zircon[J]. Geostandards and Geoanalytical Research, 2008, 32(3):247~265. doi: 10.1111/ggr.2008.32.issue-3
    [18] 柳长峰, 刘文灿, 王慧平, 等.华北克拉通北缘白乃庙组变质火山岩锆石定年与岩石地球化学特征[J].地质学报, 2014, 88(7):1273~1287. http://www.oalib.com/paper/4512353

    LIU Changfeng, LIU Wencan, WANG Huiping, et al. Geochronology and geochemistry of the bainaimiao metavolcanic rocks in the northern margin of North China Craton[J]. Acta Geologica Sinica, 2014, 88(7):1237~1287. (in Chinese with English abstract) http://www.oalib.com/paper/4512353
    [19] 路凤香, 桑隆康.岩石学[M].北京:地质出版社, 2002, 319~320.

    LU Fengxiang, SANG Longkang. Petrology[M]. Beijing:Geological Publishing House, 2002, 319~320. (in Chinese)
    [20] 周世泰.对17种恢复变质岩原岩的岩石化学方法的检验结果[J].地质论评, 1984, 30(1):81~84. https://www.wenkuxiazai.com/doc/e60cc54f376baf1ffd4fad32-2.html

    ZHOU Shitai. Examination of 17 petrochemical methods of restoring protoliths of metamorphic rocks[J]. Geological Review, 1984, 30(1):81~84. (in Chinese with English abstract) https://www.wenkuxiazai.com/doc/e60cc54f376baf1ffd4fad32-2.html
    [21] 王仁民, 贺高品, 陈珍珍, 等.变质岩原岩图解判别法[M].北京:地质出版社, 1986.

    WANG Renmin, HE Gaopin, CHEN Zhenzhen, et al. Diagrammatic identification of metamorphic rocks[M]. Beijing:Geological Publishing House, 1986. (in Chinese)
    [22] Zhou J B, Wilde S A. The crustal accretion history and tectonic evolution of the NE China segment of the Central Asian Orogenic Belt[J]. Gondwana Research, 2013, 23(4):1365~1377. doi: 10.1016/j.gr.2012.05.012
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  • 收稿日期:  2017-11-26
  • 修回日期:  2018-05-12
  • 刊出日期:  2018-08-01

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