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华北地块北缘泥盆纪岩浆活动及其构造背景

张琪琪 张拴宏

张琪琪, 张拴宏, 2019. 华北地块北缘泥盆纪岩浆活动及其构造背景. 地质力学学报, 25 (1): 125-138. DOI: 10.12090/j.issn.1006-6616.2019.25.01.012
引用本文: 张琪琪, 张拴宏, 2019. 华北地块北缘泥盆纪岩浆活动及其构造背景. 地质力学学报, 25 (1): 125-138. DOI: 10.12090/j.issn.1006-6616.2019.25.01.012
ZHANG Qiqi, ZHANG Shuanhong, 2019. DEVONIAN MAGMATISM IN THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK AND ITS TECTONIC SETTING. Journal of Geomechanics, 25 (1): 125-138. DOI: 10.12090/j.issn.1006-6616.2019.25.01.012
Citation: ZHANG Qiqi, ZHANG Shuanhong, 2019. DEVONIAN MAGMATISM IN THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK AND ITS TECTONIC SETTING. Journal of Geomechanics, 25 (1): 125-138. DOI: 10.12090/j.issn.1006-6616.2019.25.01.012

华北地块北缘泥盆纪岩浆活动及其构造背景

doi: 10.12090/j.issn.1006-6616.2019.25.01.012
基金项目: 

国家自然科学基金项目 41372230

国家自然科学基金项目 41572204

国家重点研发计划课题 2018YFC0603802

详细信息
    作者简介:

    张琪琪(1993-), 男, 在读博士, 从事构造地质与大地构造学研究。E-mail:cagszhangqiqi@163.com

    通讯作者:

    张拴宏(1974-), 男, 研究员, 从事区域地质与大地构造学研究。E-mail:tozhangshuanhong@163.com, zhangshuanhong@geomech.ac.cn

  • 中图分类号: P534.44;P588.11

DEVONIAN MAGMATISM IN THE NORTHERN MARGIN OF THE NORTH CHINA BLOCK AND ITS TECTONIC SETTING

  • 摘要: 晚古生代—早中生代岩浆岩广泛分布在华北地块北缘,构成了沿华北地块北缘呈近东—西向分布的上千公里的岩浆岩带。泥盆纪岩浆岩作为其中的组成部分,虽然分布范围不及石炭—二叠纪岩浆岩广泛,但近十多年来随着研究工作的深入,越来越多的泥盆纪岩浆岩被发现,其构造背景及意义也逐渐引起重视。对华北地块北缘近年来发现的泥盆纪岩浆活动进行总结分析表明,泥盆纪岩浆活动时限在400~360 Ma左右,其中碱性侵入岩和基性—超基性侵入岩时代主要集中在400~380 Ma之间,沿华北地块北缘自东向西均有分布;火山岩则主要集中在400 Ma和360 Ma,主要分布在华北北缘东段的赤峰地区。泥盆纪侵入岩在岩石组合上以碱性杂岩及碱性花岗岩为主,其次为二长闪长岩、基性—超基性杂岩。泥盆纪火山岩则以变质流纹质火山岩—次火山岩—火山碎屑岩及变质玄武安山岩、玄武岩(斜长角闪岩)为主,总体上具有双峰式岩石组合特征。综合研究该地区构造演化历史及泥盆纪岩石组合、弱构造变形特征、岩石地球化学与同位素地球化学组成等,认为泥盆纪岩浆活动的形成与白乃庙岛弧和华北地块在晚志留世发生弧—陆碰撞后的伸展背景有关。华北北缘泥盆纪岩浆岩带的形成对于认识古生代期间地壳增生过程、方式及古亚洲洋最终闭合时间有重要科学意义。

     

  • 图  1  华北地块泥盆纪岩浆岩分布图(据文献[18]修改)

    Figure  1.  Geological sketch map showing distribution of the Devonian magmatic rocks in the northern margin of the North China Block(Modified after reference [18])

    图  2  华北地块北缘泥盆纪侵入岩锆石U-Pb年龄分布直方图

    Figure  2.  Histogram of zircon U-Pb ages of the Devonian intrusive rocks in the northern margin of the North China Block

    图  3  华北地块北缘泥盆纪岩浆岩Nd同位素组成(数据来源于文献[19~20, 21~22, 24~25, 40~41, 43])

    Figure  3.  Nd isotopic compositions of the Devonian magmatic rocks in the northern margin of the North China Block (Data are from references [19~20, 21~22, 24~25, 40~41, 43])

    图  4  华北地块北缘泥盆纪岩浆岩Hf同位素组成(数据来源于文献[19, 21~22, 24~25, 27~28, 33, 43])

    Figure  4.  Hf isotopic compositions of the Devonian magmatic rocks in the northern margin of the North China Block (Data are from references [19, 21~22, 24~25, 27~28, 33, 43])

    表  1  华北地块北缘泥盆纪岩浆岩锆石U-Pb年龄汇总表

    Table  1.   Summary of zircon U-Pb ages of the Devonian magmatic rocks in the northern margin of the North China Block

    样品号 纬度 经度 产地 岩性 年龄/Ma 测试方法 数据来源
    侵入岩
    07169-1 40°56′17″ 110°32′54″ 白菜沟 二长岩 395±3 LA-ICP-MS [19]
    16240-1 40°56′47″ 110°32′48″ 白菜沟 二长花岗岩 402±2 LA-ICP-MS [19]
    16243-1 40°55′55″ 110°34′47″ 白菜沟 二长花岗岩 402±2 LA-ICP-MS [19]
    16245-1 40°55′44″ 110°34′46″ 白菜沟 二长花岗岩 399±3 LA-ICP-MS [19]
    P17JD1-7 高家村 角闪正长岩 390±5 TIMS [20]
    N741 41°01′34″ 110°31′05″ 高家村 角闪正长岩 399±7 SHRIMP [20]
    08587-1 41°02′35″ 110°25′17″ 高家村 角闪正长岩 396±2 LA-ICP-MS [19]
    JN07-19 三道沟 石英正长岩 409±2 LA-ICP-MS [21]
    JN08-01 三道沟 辉石正长岩 408±4 LA-ICP-MS [21]
    07052-1 41°33′23″ 112°53′30″ 三道沟 辉石正长岩 401±2 LA-ICP-MS [19]
    16206-1 41°32′59″ 112°57′42″ 三道沟 二长岩 401±1 LA-ICP-MS [19]
    16206-2 41°32′59″ 112°57′42″ 三道沟 辉长岩 399±1 LA-ICP-MS [19]
    16206-3 41°32′59″ 112°57′42″ 三道沟 辉石岩 398±2 LA-ICP-MS [19]
    NM96 乌兰哈达 石英二长岩 382±4 SHRIMP [22]
    07053-1 41°35′49″ 113°08′18″ 乌兰哈达 二长岩 381±2 LA-ICP-MS [19]
    16200-1 41°35′33″ 113°10′28″ 乌兰哈达 二长岩 379±1 LA-ICP-MS [19]
    16200-2 41°35′33″ 113°10′28″ 乌兰哈达 辉长岩 377±1 LA-ICP-MS [19]
    16200-3 41°35′33″ 113°10′28″ 乌兰哈达 辉石岩 381±5 LA-ICP-MS [19]
    DP-4 水泉沟 石英二长岩 390±6 SHRIMP [23]
    HG-1 水泉沟 正长岩 386±7 SHRIMP [23]
    H-1 下哈叭沁 异剥钙榴岩 396±5 SHRIMP [26]
    D485 41°10′17″ 117°15′58″ 红石砬 辉石岩 393±4 LA-ICP-MS [25]
    D486 41°10′13″ 117°15′52″ 红石砬 辉石岩 381±7 SHRIMP [25]
    D488 41°10′03″ 117°16′11″ 红石砬 辉石岩 388±2 LA-ICP-MS [25]
    D500 41°08′18″ 117°38′15″ 二道沟 角闪岩 395±11 SHRIMP [25]
    D496-1 41°09′17″ 117°43′02″ 下哈叭沁 异剥钙榴岩 392±5 SHRIMP [25]
    XT24-1 41°13′32″ 117°46′24″ 龙王庙 角闪岩 382±10 LA-ICP-MS [27]
    XT24-2 41°13′44″ 117°46′25″ 龙王庙 单斜辉石岩 399±4 LA-ICP-MS [27]
    D055-1 41°12′09″ 117°48′04″ 孤山 二长闪长岩 390±5 SHRIMP [24]
    2006MHS 红山 正长花岗岩 387±4 SHRIMP [28]
    15054-1 42°18′03″ 118°58′25″ 红山 正长花岗岩 388±3 LA-ICP-MS [19]
    X5 42°20′02″ 119°03′45″ 红庙子 正长花岗岩 392±2 LA-ICP-MS [29]
    15057-1 42°20′03″ 119°03′45″ 红庙子 正长花岗岩 391±4 LA-ICP-MS [19]
    BN101 42°24′53″ 119°06′43″ 鸡冠山 正长花岗斑岩 377±2 LA-ICP-MS [29]
    15062-1 42°24′35″ 119°06′46″ 鸡冠山 正长花岗斑岩 393±3 LA-ICP-MS [19]
    06C205 车户沟 正长花岗岩 376±3 LA-ICP-MS [30]
    B14 车户沟 正长花岗岩 373±6 SIMS [31]
    B231 车户沟 二长花岗岩 385±4 SIMS [31]
    火山岩
    YSH04-1 八当山 流纹质凝灰岩 404±1 LA-ICP-MS [33]
    07D013-1 42°34′09″ 119°41′53″ 赤峰莲花山 流纹质凝灰岩 366±2 LA-ICP-MS [38]
    07D014-1 42°34′13″ 119°42′02″ 赤峰莲花山 流纹质凝灰岩 364±2 LA-ICP-MS [38]
    P1TW3 42°10′30″ 121°20′40″ 朝吐沟 变质流纹岩 360±1 LA-ICP-MS [39]
    P2TW1 42°15′30″ 121°23′40″ 朝吐沟 变质流纹岩 359±1 LA-ICP-MS [39]
    下载: 导出CSV

    表  2  华北地块北缘泥盆纪岩浆岩Sr-Nd同位素汇总表

    Table  2.   Summary of Sr-Nd isotopes of the Devonian magmatic rocks in the northern margin of the North China Block

    样品号 岩石类型 年龄/Ma (87Sr/86Sr)i εNd(T) TDM(Ga) 数据来源
    白菜沟
    07169-1 二长岩 395 0.705094 -18.9 2.42 [19]
    高家村
    N0741 角闪正长岩 399 0.706067 -14.4 2.08 [20]
    N0741-1 角闪正长岩 399 0.706208 -14.9 2.15 [20]
    08586-1 二长岩 396 0.705530 -14.3 2.15 [19]
    08587-1 角闪正长岩 396 0.705592 -14.4 2.12 [19]
    三道沟
    JN07-3 石英正长岩 409 0.705473 -16.2 2.05 [21]
    JN07-8 二长岩 409 0.706155 -12.9 2.75 [21]
    JN07-9 二长岩 409 0.707445 -12.7 2.40 [21]
    JN07-18 石英正长岩 409 0.705391 -16.1 2.69 [21]
    JN07-19 石英正长岩 409 0.705261 -16.9 3.18 [21]
    JN07-23 辉石正长岩 409 0.706142 -15.1 2.14 [21]
    JN07-25 辉石正长岩 409 0.706267 -15.1 2.12 [21]
    JN07-52 辉石正长岩 409 0.706979 -17.5 2.30 [21]
    JN07-53 辉石正长岩 409 0.707056 -17.9 2.27 [21]
    07049-1 辉石正长岩 401 0.706906 -17.7 2.27 [19]
    07051-1 辉石正长岩 401 0.706237 -15.3 2.18 [19]
    07052-1 辉石正长岩 401 0.706728 -16.9 2.21 [19]
    16206-1 二长岩 401 0.707733 -9.3 1.36 [19]
    16206-2 辉长岩 399 0.707848 -10.6 1.70 [19]
    16206-3 辉石岩 398 0.707888 -10.6 1.94 [19]
    乌兰哈达
    NM98 石英二长岩 382 0.707623 -12.1 1.84 [22]
    NM99 石英二长岩 382 0.708084 -12.8 2.08 [22]
    NM101-2 石英二长岩 382 0.707680 -12.3 1.90 [22]
    07053-1 二长岩 381 0.707713 -11.8 2.06 [19]
    16200-1 二长岩 379 0.707664 -10.7 1.93 [19]
    16200-2 辉长岩 377 0.707517 -10.5 1.96 [19]
    16200-3 辉石岩 381 0.707717 -10.6 1.97 [19]
    16201-1 石英二长岩 381 0.707788 -12.2 2.01 [19]
    16201-2 辉长岩 381 0.707803 -10.9 1.92 [19]
    16201-3 辉石岩 381 0.707916 -11.8 2.21 [19]
    水泉沟
    115 角闪辉石岩 390 0.705185 -6.2 1.62 [40]
    114 暗色正长岩 390 0.704890 -7.3 1.80 [40]
    106 暗色正长岩 390 0.705450 -17.0 2.02 [40]
    T18 淡色正长岩 390 0.705171 -9.3 2.10 [40]
    T19 淡色正长岩 390 0.705204 -9.2 1.98 [40]
    N45 淡色正长岩 390 0.705076 -9.5 1.86 [40]
    N69 淡色正长岩 390 0.705274 -9.1 1.72 [40]
    N44 淡色正长岩 390 0.705186 -10.7 2.62 [40]
    N27 淡色正长岩 390 0.705158 -9.0 2.62 [40]
    N43 淡色正长岩 390 0.704944 -10.3 3.00 [40]
    N46 淡色正长岩 390 0.704860 -11.8 2.91 [40]
    80-1 淡色正长岩 390 0.705003 -10.6 2.26 [40]
    84 淡色正长岩 390 0.705204 -10.9 1.65 [40]
    80-2 白岗岩 390 0.704179 -13.2 2.55 [40]
    81 白岗岩 390 0.702233 -12.3 1.92 [40]
    82 白岗岩 390 0.702722 -13.1 2.03 [40]
    孤山
    D055-1 二长闪长岩 390 0.704885 -7.5 1.79 [24]
    D058-1 二长闪长岩 390 0.705053 -9.5 1.88 [24]
    车户沟
    CG11 正长花岗岩 376 0.709981 -21.2 2.16 [41]
    CG12 正长花岗岩 376 0.710974 -21.3 2.87 [41]
    CG13 正长花岗岩 376 0.707791 -20.9 2.45 [41]
    CG14 正长花岗岩 376 0.710357 -21.2 2.26 [41]
    CG31 二长花岗岩 376 0.708566 -19.2 2.11 [41]
    CG32 二长花岗岩 376 0.708364 -19.0 2.13 [41]
    CG33 二长花岗岩 376 0.708516 -18.9 2.05 [41]
    CG34 二长花岗岩 376 0.708625 -19.1 2.05 [41]
    冀北红石砬、二道沟、下哈叭沁
    D485 辉石岩 395 0.704672 -2.7 1.23 [25]
    D486 角闪辉石岩 395 0.704687 -1.5 1.37 [25]
    D488 辉石岩 395 0.704758 -3.4 1.39 [25]
    D492 辉石角闪岩 395 0.704787 -4.6 1.96 [25]
    D493-1 异剥钙榴岩 395 0.704735 -6.3 1.55 [25]
    D494 角闪岩 395 0.707056 -15.5 2.84 [25]
    D496-1 异剥钙榴岩 395 0.704922 -5.8 2.51 [25]
    D497 辉石岩 395 0.704915 -6.3 2.33 [25]
    D500 角闪岩 395 0.704983 -10.0 3.60 [25]
    朝吐沟
    P2Gs3 玄武岩 360 0.707748 0.5 0.99 [43]
    P2Gs12 玄武岩 360 0.705100 1.6 1.09 [43]
    P1Gs23-2 玄武岩 360 0.705975 4.9 0.94 [43]
    P2TW1 流纹岩 360 0.739739 -1.8 1.15 [43]
    P2TW2 流纹岩 360 0.725408 -1.6 1.14 [43]
    P2TW11 流纹岩 360 0.714061 -1.5 1.13 [43]
    P2TW14 流纹岩 360 0.714535 1.6 0.91 [43]
    P1Gs34 流纹岩 360 0.713906 2.5 0.84 [43]
    下载: 导出CSV

    表  3  华北地块北缘泥盆纪岩浆岩Hf同位素汇总表

    Table  3.   Summary of Hf isotopes of the Devonian magmatic rocks in the northern margin of the North China Block

    样品号 岩石类型 年龄(Ma) εHf(T) TDM(Ga) TDMC(Ga) 数据来源
    白菜沟
    07169-1 二长岩 395 -34.1~-24.8 2.34~2.00 3.52~2.94 [19]
    16240-1 二长花岗岩 402 -34.1~-12.0 2.34~1.54 3.52~2.16 [19]
    16243-1 二长花岗岩 402 -26.8~-13.0 2.12~1.59 3.07~2.21 [19]
    16245-1 二长花岗岩 399 -25.0~-14.6 2.03~1.62 2.96~2.31 [19]
    高家村
    08587-1 角闪正长岩 396 -20.5~-17.5 1.81~1.71 2.68~2.53 [19]
    三道沟
    JN07-19 石英正长岩 409 -31.5~-26.8 2.28~2.05 3.37~3.08 [21]
    JN08-1 辉石正长岩 409 -32.3~-28.1 2.27~2.11 3.42~3.16 [21]
    07052-1 辉石正长岩 401 -32.2~-29.1 2.27~2.16 3.40~3.24 [19]
    16206-1 二长岩 401 -21.9~-13.9 1.88~1.57 2.77~2.27 [19]
    16206-2 辉长岩 399 -24.4~-15.1 1.97~1.60 2.92~2.35 [19]
    16206-3 辉石岩 398 -23.1~-17.2 1.92~1.69 2.84~2.48 [19]
    乌兰哈达
    NM96-1 石英二长岩 382 -23.4~-17.2 1.94~1.67 2.85~2.46 [22]
    07053-1 二长岩 381 -22.2~-15.5 1.87~1.63 2.77~2.36 [19]
    16200-1 二长岩 379 -22.1~-18.1 2.08~1.71 2.76~2.51 [19]
    16200-2 辉长岩 377 -24.3~-17.4 1.95~1.66 2.90~2.46 [19]
    16200-3 辉石岩 381 -23.6~-16.0 1.93~1.64 2.86~2.40 [19]
    孤山
    D055-1 二长闪长岩 390 -12.0~-5.8 1.48~1.23 2.14~1.75 [24]
    赤峰红山
    2006MHS 钾长花岗岩 387 -11.5~-8.5 1.54~1.38 2.11~1.92 [28]
    15054-1 正长花岗岩 388 -15.6~-8.3 1.66~1.35 2.36~1.91 [19]
    赤峰红庙子
    15057-1 正长花岗岩 391 -17.3~-8.2 1.74~1.36 2.48~1.91 [19]
    赤峰车户沟
    06C205 正长花岗岩 376 -44.4~-20.5 2.71~1.81 4.12~2.66 [19]
    龙王庙
    XT24-1 角闪岩 382 -13.2~-11.8 1.52~1.45 2.21~2.12 [27]
    XT24-2 辉石岩 399 -15.1~-9.8 1.60~1.39 2.34~2.01 [27]
    冀北红石砬、二道沟、下哈叭沁
    D485 辉石岩 395 -3.8~5.5 1.18~0.80 1.63~1.04 [25]
    D486 角闪辉石岩 395 0.5~1.2 1.01~0.99 1.36~1.31 [25]
    D488 辉石岩 395 -4.4~-0.4 1.17~1.02 1.67~1.42 [25]
    D496-1 异剥钙榴岩 395 -11.5~-6.5 1.45~1.26 2.12~1.80 [25]
    D500 角闪岩 395 -10.9~-4.1 1.47~1.23 2.08~1.65 [25]
    八当山
    YSH04-1 流纹质凝灰岩 404 -22.0~-16.4 1.94~1.69 2.78~2.43 [33]
    朝吐沟
    P1TW3 流纹岩 360 -1.0~5.7 1.03~0.77 1.43~1.00 [43]
    P2TW1 流纹岩 360 -1.9~5.3 1.07~0.78 1.49~1.03 [43]
    下载: 导出CSV
  • [1] Liu D Y, Nutman A P, Compston W, et al. Remnants of ≥ 3800 Ma crust in the Chinese part of the Sino-Korean Craton[J]. Geology, 1992, 20(4):339~342. doi: 10.1130/0091-7613(1992)020<0339:ROMCIT>2.3.CO;2
    [2] Zhao G C, Sun M, Wilde S A, et al. Late archean to paleoproterozoic evolution of the North China Craton:key issues revisited[J]. Precambrian Research, 2005, 136(2):177~202. doi: 10.1016/j.precamres.2004.10.002
    [3] Zhai M G. Cratonization and the Ancient North China continent:a summary and review[J]. Science China Earth Sciences, 2011, 54(8):1110~1120. doi: 10.1007/s11430-011-4250-x
    [4] 吴福元, 徐义刚, 高山, 等.华北岩石圈减薄与克拉通破坏研究的主要学术争论[J].岩石学报, 2008, 24(6):1145~1174. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200806001

    WU Fuyuan, XU Yigang, GAO Shan, et al. Lithospheric thinning and destruction of the North China Craton[J]. Acta Petrologica Sinica, 2008, 24(6):1145~1174. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/ysxb98200806001
    [5] 徐义刚, 李洪颜, 庞崇进, 等.论华北克拉通破坏的时限[J].科学通报, 2009, 54(14):1974~1989. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=CAS201303040000253705

    XU Yigang, LI Hongyan, PANG Chongjin, et al. On the timing and duration of the destruction of the North China Craton[J]. Chinese Science Bulletin, 2009, 54(19):3379~3396. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=CAS201303040000253705
    [6] 朱日祥, 徐义刚, 朱光, 等.华北克拉通破坏[J].中国科学:地球科学, 2012, 42(8):1135~1159. http://d.old.wanfangdata.com.cn/Periodical/ddgzyckx200804016

    ZHU Rixiang, XU Yigang, ZHU Guang, et al. Destruction of the North China Craton[J]. Science China Earth Sciences, 2012, 55(10):1565~1587. http://d.old.wanfangdata.com.cn/Periodical/ddgzyckx200804016
    [7] 王荃, 刘雪亚, 李锦轶.中国华夏与安加拉古陆间的板块构造[M].北京:北京大学出版社, 1991.

    WANG Quan, LIU Xueya, LI Jinyi. Plate tectonics between cathaysia and angaraland in China[M]. Beijing:Peking University Press, 1991. (in Chinese)
    [8] Xiao W J, Windley B F, Hao J, et al. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China:Termination of the central Asian orogenic belt[J]. Tectonics, 2003, 22(6):1069. http://www.oalib.com/references/19006779
    [9] 李锦轶, 张进, 杨天南, 等.北亚造山区南部及其毗邻地区地壳构造分区与构造演化[J].吉林大学学报(地球科学版), 2009, 39(4):584~605. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb200904002

    LI Jinyi, ZHANG Jin, YANG Tiannan, et al. Crustal tectonic division and evolution of the southern part of the North Asian Orogenic region and its adjacent areas[J]. Journal of Jilin University (Earth Science Edition), 2009, 39(4):584~605. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb200904002
    [10] Hsu K J, Wang Q, Hao J. Geologic evolution of the Neimonides:a working hypothesis[J]. Eclogae Geologicae Helvetiae, 1991, 84(1):1~31.
    [11] 唐克东.中朝板块北侧褶皱带构造演化及成矿规律[M].北京:北京大学出版社, 1992.

    TANG Kedong. Tectonic evolution and minerogenetic regularities of the fold belt along the northern margins of Sino-Korean plate[M]. Beijing:Peking University Press, 1992. (in Chinese)
    [12] 徐备, 陈斌.内蒙古北部华北板块与西伯利亚板块之间中古生代造山带的结构及演化[J].中国科学(D辑), 1997, 27(3):227~232. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700269956

    XU Bei, CHEN Bin. Framework and evolution of the middle Paleozoic orogenic belt between Siberian and North China plates in northern Inner Mongolia[J]. Science in China (Series D), 1997, 40(5):463~469. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700269956
    [13] 程胜东, 方俊钦, 赵盼, 等.内蒙古西拉木伦河两岸志留-泥盆系碎屑锆石年龄及其构造意义[J].岩石学报, 2014, 30(7):1909~1921. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201407007

    CHENG Shengdong, FANG Junqin, ZHAO Pan, et al. Detrital zircon ages of the Silurian-Devonian clastic rocks in south and north banks of Xar Moron River, Inner Mongolia[J]. Acta Petrologica Sinica, 2014, 30(7):1909~1921. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/ysxb98201407007
    [14] 李锦轶, 高立明, 孙桂华, 等.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[J].岩石学报, 2007, 23(3):565~582. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200703004

    LI Jinyi, GAO Liming, SUN Guihua, et al. 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[J]. Acta Petrologica Sinica, 2007, 23(3):565~582. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/ysxb98200703004
    [15] 李钢柱, 王玉净, 李成元, 等.内蒙古索伦山蛇绿岩带早二叠世放射虫动物群的发现及其地质意义[J].科学通报, 2017, 62(5):400~406. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QKC20172017031700121596

    LI Gangzhu, WANG Yujing, LI Chengyuan, et al. Discovery of Early Permian radiolarian fauna in the Solon Obo ophiolite belt, Inner Mongolia and its geological significance[J]. Chinese Science Bulletin, 2017, 62(5):400~406. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QKC20172017031700121596
    [16] 郭伟, 杨欣德, 张娟, 等.内蒙古赤峰北部下二叠统于家北沟组碎屑沉积岩地球化学特征[J].地质力学学报, 2011, 17(3):295~302. doi: 10.3969/j.issn.1006-6616.2011.03.009

    GUO Wei, YANG Xinde, ZHANG Juan, et al. Geochemical characteristics of clastic sedimentary rocks from lower Permian Yujiabeigou Formation in northern Chifeng, Inner Mongolia[J]. Journal of Geomechanics, 2011, 17(3):295~302. (in Chinese with English abstract) doi: 10.3969/j.issn.1006-6616.2011.03.009
    [17] Şengör A M C, Natal'in B A, Burtman V S. Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia[J]. Nature, 1993, 364(6435):299~307. doi: 10.1038/364299a0
    [18] 张拴宏, 赵越, 刘健民, 等.华北地块北缘晚古生代-早中生代岩浆活动期次、特征及构造背景[J].岩石矿物学杂志, 2010, 29(6):824~842. doi: 10.3969/j.issn.1000-6524.2010.06.017

    ZHANG Shuanhong, ZHAO Yue, LIU Jianmin, et al. Geochronology, geochemistry and tectonic setting of the Late Paleozoic-Early Mesozoic magmatism in the northern margin of the North China Block:a preliminary review[J]. Acta Petrologica et Mineralogica, 2010, 29(6):824~842. (in Chinese with English abstract) doi: 10.3969/j.issn.1000-6524.2010.06.017
    [19] Zhang Q Q, Zhang S H, Zhao Y, et al. Devonian alkaline magmatic belt along the northern margin of the North China Block:petrogenesis and tectonic implications[J]. Lithos, 2018, 302~303:496~518. https://www.sciencedirect.com/science/article/pii/S002449371830029
    [20] 王惠初, 相振群, 赵凤清, 等.内蒙古固阳东部碱性侵入岩:年代学、成因与地质意义[J].岩石学报, 2012, 28(9):2843~2854. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201209014

    WANG Huichu, XIANG Zhenqun, ZHAO Fengqing, et al. The alkaline plutons in eastern part of Guyang county, Inner Mongolia:geochronology, petrogenesis and tectonic implications[J]. Acta Petrologica Sinica, 2012, 28(9):2843~2854. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/ysxb98201209014
    [21] Zhang X H, Zhang H F, Jiang N, et al. Early Devonian alkaline intrusive complex from the northern North China Craton:a petrological monitor of post-collisional tectonics[J]. Journal of the Geological Society, 2010, 167(4):717~730. doi: 10.1144/0016-76492009-110
    [22] Huang D L, Hou, Q Y. Devonian alkaline magmatism in the northern North China Craton:geochemistry, SHRIMP zircon U-Pb geochronology and Sr-Nd-Hf isotopes[J]. Geoscience Frontiers, 2017, 8(1):171~181. doi: 10.1016/j.gsf.2016.02.006
    [23] 罗镇宽, 苗来成, 关康, 等.河北张家口水泉沟岩体SHRIMP年代学研究及其意义[J].地球化学, 2001, 30(2):116~122. doi: 10.3321/j.issn:0379-1726.2001.02.002

    LUO Zhenkuan, MIAO Laicheng, GUAN Kang, et al. SHRIMP chronological study of Shuiquangou intrusive body in Zhangjiakou area, Hebei province and its geochemical significance[J]. Geochimica, 2001, 30(2):116~122. (in Chinese with English abstract) doi: 10.3321/j.issn:0379-1726.2001.02.002
    [24] Zhang S H, Zhao Y, Song B, et al. Petrogenesis of the middle Devonian Gushan diorite pluton on the northern margin of the North China block and its tectonic implications[J]. Geological Magazine, 2007, 144(3):553~568. doi: 10.1017/S0016756807003275
    [25] Zhang S H, Zhao Y, Liu X C, et al. Late Paleozoic to Early Mesozoic mafic-ultramafic complexes from the northern North China Block:constraints on the composition and evolution of the lithospheric mantle[J]. Lithos, 2009, 110(1/4):229~246. http://www.sciencedirect.com/science/article/pii/S002449370900022X
    [26] 倪志耀.冀北退变榴辉岩、异剥钙榴岩和变质橄榄岩及其地质意义[D].北京: 中国科学院地质与地球物理研究所, 2002, 1~83. http://www.wanfangdata.com.cn/details/detail.do?_type=degree&id=Y469211

    NI Zhiyao. Retrograded eclogites, rodingites and metamorphic periodtites and their geotectonic significance in the northern margin of the North China Craton, Hebei province, China[D]. Beijing: Institute of Geology And Geophysics Chinese Academy of Sciences, 2002, 1~83. (in Chinese) http://www.wanfangdata.com.cn/details/detail.do?_type=degree&id=Y469211
    [27] Teng X M, Yang Q Y, Santosh M. Devonian magmatism associated with arc-continent collision in the northern North China Craton:evidence from the Longwangmiao ultramafic intrusion in the Damiao area[J]. Journal of Asian Earth Sciences, 2015, 113:626~643. doi: 10.1016/j.jseaes.2015.04.032
    [28] Shi Y R, Liu D Y, Miao L C, et al. Devonian A-type granitic magmatism on the northern margin of the North China Craton:SHRIMP U-Pb zircon dating and Hf-isotopes of the Hongshan granite at Chifeng, Inner Mongolia, China[J]. Gondwana Research, 2010, 17(4):632~641. doi: 10.1016/j.gr.2009.11.011
    [29] 徐博文, 郗爱华, 葛玉辉, 等.内蒙古赤峰地区晚古生代A型花岗岩锆石U-Pb年龄及构造意义[J].地质学报, 2015, 89(1):58~69. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201501005

    XU Bowen, XI Aihua, GE Yuhui, et al. Zircon U-Pb ages of the Late Paleozoic A-type granites in Chifeng, Inner Mongolia and its tectonic significance[J]. Acta Geologica Sinica, 2015, 89(1):58~69. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/dizhixb201501005
    [30] Liu J M, Zhao Y, Sun Y L, et al. Recognition of the latest Permian to Early Triassic Cu-Mo mineralization on the northern margin of the North China block and its geological significance[J]. Gondwana Research, 2010, 17(1):125~134. doi: 10.1016/j.gr.2009.07.007
    [31] Zeng Q D, Yang J H, Liu J M, et al. Genesis of the Chehugou Mo-bearing granitic complex on the northern margin of the North China Craton:geochemistry, zircon U-Pb age and Sr-Nd-Pb isotopes[J]. Geological Magazine, 2012, 149(5):753~767. doi: 10.1017/S0016756811000987
    [32] 内蒙古地质矿产局. 1: 20万敖汉旗幅(K-50-ⅩⅧ)区域地质调查报告[R]. 1970.

    Bureau of Geology and Mineral Resources of Inner Mongolia. Geological Map of Aohanqi (K-50-ⅩⅧ): Inner Mongolia, Bureau of Geology and Mineral Resources of Inner Mongolia, Scale 1: 200000[R]. 1970. (in Chinese)
    [33] 刘建峰, 李锦轶, 迟效国, 等.华北克拉通北缘与弧-陆碰撞相关的早泥盆世长英质火山岩——锆石U-Pb定年及地球化学证据[J].地质通报, 2013, 32(2/3):267~278. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201302006

    LIU Jianfeng, LI Jinyi, CHI Xiaoguo, et al. Early Devonian felsic volcanic rocks related to the arc-continent collision on the northern margin of North China Craton-evidences of zircon U-Pb dating and geochemical characteristics[J]. Geological Bulletin of China, 2013, 32(2/3):267~278. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201302006
    [34] 内蒙古自治区地质矿产局.内蒙古自治区区域地质志[M].北京:地质出版社, 1991.

    Bureau of Geology and Mineral Resources of Inner Mongolia. Region geology of Inner Mongolia autonomous region[M]. Beijing:Geological Publishing House, 1991. (in Chinese)
    [35] 内蒙古自治区地质矿产局.内蒙古1: 20万下洼幅(K-51-XVⅢ)区域地质调查报告[R]. 1967.

    Bureau of Geology and Mineral Resources of Inner Mongolia. Geological map of Xiawa (K-51-XVⅢ): Inner Mongolia, bureau of geology and mineral resources of Inner Mongolia, scale 1: 200000[R]. 1967. (in Chinese)
    [36] 辽宁省地质矿产局.辽宁1: 20万阜新幅(K-51-XIV)区域地质调查报告[R]. 1971.

    Bureau of Geology and Mineral Resources of Liaoning Province. Geological map of Fuxin (K-51-XIV): Liaoning, bureau of geology and mineral resources of Liaoning Province, Scale 1: 200000[R]. 1971. (in Chinese)
    [37] 胡泽瑾.内蒙古昭乌达盟朝吐沟组时代应为泥盆纪[J].中国区域地质, 1983, (6):141. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000005065532

    HU Zejin. Age of the Chaotugou formation in Ju Ud League in Inner Mongolia should be Devonian[J]. Regional Geology of China, 1983, (6):141. (in Chinese) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000005065532
    [38] 叶浩, 张拴宏, 赵越, 等.内蒙古赤峰地区泥盆纪晚期火山岩的发现及其地质意义[J].地质通报, 2014, 33(9):1274~1283. doi: 10.3969/j.issn.1671-2552.2014.09.002

    YE Hao, ZHANG Shuanhong, ZHAO Yue, et al. Recognition of the latest Devonian volcanic rocks in Chifeng area, northern North China block, and its geological implications[J]. Geological Bulletin of China, 2014, 33(9):1274~1283. (in Chinese with English abstract) doi: 10.3969/j.issn.1671-2552.2014.09.002
    [39] 孙立新, 任邦方, 滕飞, 等.内蒙古敖汉旗朝吐沟组火山岩LA-ICP-MS锆石U-Pb年龄[J].地质通报, 2015, 34(8):1493~1501. doi: 10.3969/j.issn.1671-2552.2015.08.009

    SUN Lixin, REN Bangfang, TENG Fei, et al. LA-ICP-MS zircon U-Pb ages of the volcanoic rocks from the Chao-tugou Formation in Aohan Banner, Inner Mongolia[J]. Geological Bulletin of China, 2015, 34(8):1493~1501. (in Chinese with English abstract) doi: 10.3969/j.issn.1671-2552.2015.08.009
    [40] Jiang N. Petrology and geochemistry of the Shuiquangou syenitic complex, northern margin of the North China Craton[J]. Journal of the Geological Society, 2005, 162(1):203~215. doi: 10.1144/0016-764903-144
    [41] Wan B, Hegner E, Zhang L C, et al. Rb-Sr geochronology of chalcopyrite from the Chehugou porphyry Mo-Cu deposit (Northeast China) and geochemical constraints on the origin of hosting granites[J]. Economic Geology, 2009, 104(3):351~363. doi: 10.2113/gsecongeo.104.3.351
    [42] 张拴宏, 赵越, 刘健, 等.华北地块北缘晚古生代-中生代花岗岩体侵位深度及其构造意义[J].岩石学报, 2007, 23(3):625~638. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200703010

    ZHANG Shuanhong, ZHAO Yue, LIU Jian, et al. Emplacement depths of the Late Paleozoic-Mesozoic granitoid intrusions from the northern North China block and their tectonic implications[J]. Acta Petrologica Sinica, 2007, 23(3):625~638. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/ysxb98200703010
    [43] 孙立新, 张云, 李影, 等.内蒙古赤峰地区晚泥盆世双峰式火山岩地球化学特征与板内伸展事件[J].中国地质, 2017, 44(2):371~388. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi201702012

    SUN Lixin, ZHANG Yun, LI Ying, et al. Geochemical characteristics and intraplate extension of Late Devonian bimodal volcanic rocks in Chifeng area of Inner Mongolia[J]. Geology in China, 2017, 44(2):371~388. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/zgdizhi201702012
    [44] Smith I E M, White A J R, Chappell B W, et al. Fractionation in a zoned monzonite pluton:mount Dromedary, southeastern Australia[J]. Geological Magazine, 1988, 125(3):273~284. doi: 10.1017/S0016756800010219
    [45] Tchameni R, Mezger K, Nsifa N E, et al. Crustal origin of early Proterozoic syenites in the Congo Craton (Ntem Complex), South Cameroon[J]. Lithos, 2001, 57(1):23~42. https://www.researchgate.net/publication/221956320_Crustal_origin_of_Early_Proterozoic_syenites_in_the_Congo_Craton_Ntem_Complex_South_Cameroon
    [46] Martin R F. A-type granites of crustal origin ultimately result from open-system fenitization-type reactions in an extensional environment[J]. Lithos, 2006, 91(1/4):125~136. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=92df92c7ead8fbd1f4856844359d8423
    [47] Bonin B. Alkaline rocks and geodynamics[J]. Turkish Journal of Earth Sciences, 1998, 7:105~118. http://d.old.wanfangdata.com.cn/NSTLQK/NSTL_QKJJ0211812370/
    [48] Yang J H, Sun J F, Zhang M, et al. Petrogenesis of silica-saturated and silica-undersaturated syenites in the northern North China Craton related to post-collisional and intraplate extension[J]. Chemical Geology, 2012, 328:149~167. doi: 10.1016/j.chemgeo.2011.09.011
    [49] Xu H J, Zhang J F, Wang Y F, et al. Late Triassic alkaline complex in the Sulu UHP terrane:implications for post-collisional magmatism and subsequent fractional crystallization[J]. Gondwana Research, 2016, 35:390~410. doi: 10.1016/j.gr.2015.05.017
    [50] Paterson S R, Vernon R H, Tobisch O T. A review of criteria for the identification of magmatic and tectonic foliations in granitoids[J]. Journal of Structural Geology, 1989, 11(3):349~363. doi: 10.1016/0191-8141(89)90074-6
    [51] Vernon R H. Review of microstructural evidence of magmatic and solid-state flow[J]. Visual Geosciences, 2000, 5(2):1~23. doi: 10.1007/s10069-000-0002-3
    [52] Žak J, Verner K, Holub F V, et al. Magmatic to solid state fabrics in syntectonic granitoids recording Early Carboniferous orogenic collapse in the Bohemian Massif[J]. Journal of Structural Geology, 2012, 36:27~42. doi: 10.1016/j.jsg.2011.12.011
    [53] Zhang S H, Zhao Y. Mid-crustal emplacement and deformation of plutons in an Andean-style continental arc along the northern margin of the North China Block and tectonic implications[J]. Tectonophysics, 2013, 608:176~195. doi: 10.1016/j.tecto.2013.09.036
    [54] 吴飞, 张拴宏, 赵越, 等.华北地块北缘内蒙古固阳地区早二叠世岩体的侵位深度及其构造意义[J].中国地质, 2014, 41(3):824~837. doi: 10.3969/j.issn.1000-3657.2014.03.011

    WU Fei, ZHANG Shuanhong, ZHAO Yue, et al. Emplacement depths of the Early Permian plutons from Guyang area in the northern margin of the North China Block and their tectonic implications[J]. Geology in China, 2014, 41(3):824~837. (in Chinese with English abstract) doi: 10.3969/j.issn.1000-3657.2014.03.011
    [55] 赵越, 陈斌, 张拴宏, 等.华北克拉通北缘及邻区前燕山期主要地质事件[J].中国地质, 2010, 37(4):900~915. doi: 10.3969/j.issn.1000-3657.2010.04.007

    ZHAO Yue, CHEN Bin, ZHANG Shuanhong, et al. Pre-Yanshanian geological events in the northern margin of the North China Craton and its adjacent areas[J]. Geology in China, 2010, 37(4):900~915. (in Chinese with English abstract) doi: 10.3969/j.issn.1000-3657.2010.04.007
    [56] Zhang S H, Zhao Y, Ye H, et al. Origin and evolution of the Bainaimiao arc belt:Implications for crustal growth in the southern Central Asian Orogenic Belt[J]. Geological Society of America Bulletin, 2014, 126(9/10):1275~1300. http://www.crossref.org/iPage?doi=10.1130/B31042.1
    [57] Chao E C T, Back J M, Minkin J A, et al. The sedimentary carbonate-hosted giant Bayan Obo REE-Fe-Nb ore deposit of Inner Mongolia, China: a cornerstone example for giant polymetallic ore deposits of hydrothermal origin[R]. Washington, DC: U.S. Government Printing Office, 1994, 2143.
    [58] 刘敦一, 简平, 张旗, 等.内蒙古图林凯蛇绿岩中埃达克岩SHRIMP测年:早古生代洋壳消减的证据[J].地质学报, 2003, 77(3):317~327. doi: 10.3321/j.issn:0001-5717.2003.03.004

    LIU Dunyi, JIAN Ping, ZHANG Qi, et al. SHRIMP dating of adakites in the Tulingkai ophiolite, Inner Mongolia:evidence for the Early Paleozoic subduction[J]. Acta Geologica Sinica, 2003, 77(3):317~327. (in Chinese with English abstract) doi: 10.3321/j.issn:0001-5717.2003.03.004
    [59] 许立权, 邓晋福, 陈志勇, 等.内蒙古达茂旗北部奥陶纪埃达克岩类的识别及其意义[J].现代地质, 2003, 17(4):428~434. doi: 10.3969/j.issn.1000-8527.2003.04.011

    XU Liquan, DENG Jinfu, CHEN Zhiyong, et al. The identification of Ordovician adakites and its signification in northern Damao, Inner Mongolia[J]. Geoscience, 2003, 17(4):428~434. (in Chinese with English abstract) doi: 10.3969/j.issn.1000-8527.2003.04.011
    [60] Jian P, Liu D Y, Kröner A, et al. Time scale of an Early to Mid-Paleozoic orogenic cycle of the long-lived Central Asian Orogenic Belt, Inner Mongolia of China:Implications for continental growth[J]. Lithos, 2008, 101(3/4):233~259. http://www.sciencedirect.com/science/article/pii/S0024493707001508
    [61] 苏养正.内蒙古草原地层区的古生代地层[J].吉林地质, 1996, 15(3/4):42~54. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600282489

    SU Yangzheng. Paleozoic stratigraphy of Nei Mongol grass stratigraphical province[J]. Jilin Geology, 1996, 15(3/4):42~54. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600282489
    [62] 张允平, 苏养正, 李景春.内蒙古中部地区晚志留世西别河组的区域构造学意义[J].地质通报, 2010, 29(11):1599~1605. doi: 10.3969/j.issn.1671-2552.2010.11.001

    ZHANG Yunping, SU Yangzheng, LI Jingchun. Regional tectonics significance of the Late Silurian Xibiehe Formation in central Inner Mongolia, China[J]. Geological Bulletin of China, 2010, 29(11):1599~1605. (in Chinese with English abstract) doi: 10.3969/j.issn.1671-2552.2010.11.001
    [63] 王平.内蒙古达茂旗巴特敖包地区的西别河剖面与西别河组[J].吉林大学学报(地球科学版), 2005, 35(4):409~415. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb200504001

    WANG Ping. The Xibiehe section and Xibiehe Formation of the Bateaobao area in Darhan Mumingan Joint Banner, Inner Mongolia[J]. Journal of Jilin University (Earth Science Edition), 2005, 35(4):409~415. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb200504001
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  • 收稿日期:  2017-08-22
  • 修回日期:  2018-10-11
  • 刊出日期:  2019-02-01

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