兴蒙造山带南缘早—中二叠世砂岩碎屑锆石U-Pb年龄、Hf同位素组成及其构造意义

朱俊宾, 和政军. 兴蒙造山带南缘早—中二叠世砂岩碎屑锆石U-Pb年龄、Hf同位素组成及其构造意义[J]. 地质通报, 2017, 36(2-3): 357-371.
引用本文: 朱俊宾, 和政军. 兴蒙造山带南缘早—中二叠世砂岩碎屑锆石U-Pb年龄、Hf同位素组成及其构造意义[J]. 地质通报, 2017, 36(2-3): 357-371.
ZHU Junbin, HE Zhengjun. Detrital zircon U-Pb ages and Hf isotopes of Early-Middle Permian sandstones from the south margin of Xing-Meng orogenic belt and their tectonic significance[J]. Geological Bulletin of China, 2017, 36(2-3): 357-371.
Citation: ZHU Junbin, HE Zhengjun. Detrital zircon U-Pb ages and Hf isotopes of Early-Middle Permian sandstones from the south margin of Xing-Meng orogenic belt and their tectonic significance[J]. Geological Bulletin of China, 2017, 36(2-3): 357-371.

兴蒙造山带南缘早—中二叠世砂岩碎屑锆石U-Pb年龄、Hf同位素组成及其构造意义

  • 基金项目:
    中国地质调查局项目《中国及邻区海陆大地构造研究》(编号:DD20160343(121201102000150009))
详细信息
    作者简介: 朱俊宾(1984-),男,博士,工程师,从事大地构造研究。E-mail:zhujunbin0819@163.com
  • 中图分类号: P534.46;P588.21

Detrital zircon U-Pb ages and Hf isotopes of Early-Middle Permian sandstones from the south margin of Xing-Meng orogenic belt and their tectonic significance

  • 利用LA-MC-ICP-MS 分析技术,对兴蒙造山带南缘下二叠统三面井组和中二叠统额里图组砂岩中的碎屑锆石进行了U-Pb 年龄和Hf 同位素研究。结果显示,三面井组砂岩记录了3 组碎屑锆石年龄:280~369Ma(4 颗)、1800~2271Ma(43 颗,峰值1877Ma)和2507~2711Ma(9 颗)。额里图组砂岩碎屑锆石年龄集中分布在271~371Ma(9 颗)、1258~1395Ma(18 颗,峰值1326Ma)和1695~2454Ma(34 颗,峰值1864Ma)3 个年龄区间。对比研究发现,样品中的元古宙和太古宙碎屑锆石是华北克拉通古老基底的反映;晚古生代锆石具有较低的εHf(t)值(-5.3~-23.7)和较老的Hf 模式年龄(1124~3039Ma),与华北克拉通北缘晚古生代岩浆岩具有一致性,而明显区别于兴蒙造山带内岩浆岩Hf 同位素特征,说明前者是其物源供给区。结合区域资料认为,华北克拉通北缘在早―中二叠世期间不存在类似安第斯型的俯冲大陆边缘,三面井组和额里图组砂岩是在伸展背景下沉积形成的。

  • 加载中
  • 图 1  研究区地质简图

    Figure 1. 

    图 2  正镶白旗南部三面井组和额里图组实测剖面

    Figure 2. 

    图 3  三面井组(a、c)和额里图组(b、d)野外照片及砂岩样品显微照片

    Figure 3. 

    图 4  三面井组和额里图组砂岩部分代表性碎屑锆石CL 图像(实线圆圈表示U-Pb 测点位置,虚线圆圈表示Hf 同位素测点位置, 下面数字为Hf 同位素值)

    Figure 4. 

    图 5  三面井组和额里图组砂岩碎屑锆石U-Pb 谐和图和年龄频率分布图

    Figure 5. 

    图 6  三面井组和额里图组砂岩碎屑锆石t-εHf(t)图解

    Figure 6. 

    表 1  三面井组和额里图组砂岩LA-ICP-MS 锆石U-Th-Pb 分析结果

    Table 1.  Results of LA-ICP-MS zircon U-Th-Pb dating for the sandstonesfrom the Sanmianjing Formation and Elitu Formation

    样品号
    测点号
    PbU232Th/238U同位素比值年龄/Ma
    /10-6206Pb/238U207Pb/235U207Pb/206Pb206Pb/238U207Pb/235U207Pb/206Pb
    样品号14SMJ4
    12114760.79560.35910.00366.0280.0830.12170.0015197820198027198221
    22517640.24070.31510.00334.8520.0670.11170.0013176618179425182721
    31443980.26190.34840.00355.6870.0760.11840.0014192719192926193221
    4153030.47530.04440.00050.31750.00990.05190.00162803280927970
    5391020.51330.33850.00345.3250.0750.11410.0014188019187326186523
    6641720.45940.33600.00345.2780.0720.11390.0014186819186525186322
    7771350.62670.47840.004810.960.150.16610.0020252025252034251920
    81514570.04230.33320.00335.3310.0730.11600.0014185418187426189622
    91474140.15740.34870.00355.7610.0790.11980.0014192819194126195421
    102084471.16730.37290.00398.3090.110.16160.0019204321226531247220
    11611110.54910.47650.004810.890.150.16580.0020251225251434251620
    121634650.25190.33940.00345.4040.0710.11550.0014188419188525188821
    131574330.34230.34480.00355.5560.0750.11690.0014191019190926190921
    141373270.45500.38480.00396.8950.0930.12990.0015209921209828209721
    152734830.77570.47320.005210.950.160.16780.0020249828251936253620
    161143390.23120.33040.00335.2490.0720.11520.0014184119186126188322
    171283380.69820.33470.00355.2590.0730.11400.0014186119186226186322
    1829310170.38690.28180.00284.8280.0650.12420.0015160116179024201821
    192406900.36640.33230.00345.2080.0710.11370.0013185019185425185921
    201264380.48270.27730.00294.6290.0640.12110.0014157817175524197221
    211744920.59020.32490.00335.0180.0670.11200.0013181418182224183321
    22772030.86800.32880.00345.1480.0700.11350.0013183319184425185721
    23122360.52880.04840.00050.34850.0120.05220.001730533041029373
    24822400.45080.32570.00345.0180.0700.11180.0013181719182225182822
    25722070.62110.32160.00334.9330.0690.11120.0013179819180825182022
    26243461.18320.05830.00060.43330.00860.05390.00103664366736642
    27421200.56290.32500.00335.0790.0700.11340.0014181418183325185422
    28822170.92370.32480.00335.0560.0680.11290.0013181318182925184721
    29152460.44670.05890.00060.44360.0120.05460.001436943731039657
    30831730.31180.44830.004510.230.140.16550.0019238824245633251320
    311393610.86280.33320.00345.2950.0710.11530.0014185419186825188421
    321986120.31580.31560.00315.0450.0680.11590.0014176817182724189421
    331494230.10870.35310.00365.8370.0800.11990.0014194920195227195421
    34771950.81890.33690.00345.4000.0740.11620.0014187219188526189921
    351905340.40290.33930.00356.1350.0840.13110.0015188319199527211321
    362134010.56160.46270.004710.880.150.17050.0020245225251334256220
    37931660.58460.49000.005111.560.160.17110.0020257127257035256920
    38812260.43260.33480.00345.3250.0730.11530.0014186219187326188522
    391745250.09010.33500.00345.3420.0750.11560.0014186319187626189022
    40992241.33860.33180.00335.2480.0730.11470.0014184719186026187622
    411644330.67200.33010.00335.1840.0710.11390.0014183918185025186222
    样品号14SMJ4
    423188030.49440.35880.00365.9390.0800.12010.0014197620196727195721
    431163180.44080.33590.00345.3100.0720.11470.0014186719187025187521
    443779900.55720.34340.00375.5250.0760.11670.0014190320190526190621
    45451170.71710.33500.00335.3690.0740.11620.0014186319188026189922
    4641990.91190.34160.00355.5350.0780.11750.0015189419190627191923
    471103280.70680.30230.00344.8390.0700.11610.0014170319179226189721
    481624530.26590.34570.00365.6140.0780.11780.0014191420191827192322
    49511181.14660.34900.00365.7020.0810.11850.0015193020193227193422
    501273780.49340.31760.00335.4820.0760.12520.0015177818189826203121
    51912550.29010.35130.00365.9010.0800.12180.0014194120196127198321
    523425751.38460.46020.004610.470.140.16500.0019244024247733250820
    532117080.09130.30200.00314.6980.0640.11280.0013170118176724184621
    541313930.16890.33560.00345.2760.0720.11400.0013186519186525186521
    551712481.24320.52440.005413.480.190.18650.0022271828271437271119
    56551560.34200.33890.00355.3850.0780.11520.0015188219188227188323
    57411150.52490.32370.00334.9310.0750.11050.0015180818180828180725
    581654550.76150.32060.00335.0610.0690.11450.0013179319183025187221
    591734110.04840.42100.00458.3330.120.14360.0017226524226833227120
    60732070.51540.32420.00334.9200.0680.11010.0013181018180625180022
    611353870.38550.33440.00365.3190.0730.11530.0014186020187226188521
    622464670.56120.47000.004810.690.150.16500.0020248425249734250720
    样品号14ELT3
    1913850.42410.22640.00222.6410.0370.08460.0011131613131218130724
    2341430.46060.22050.00222.5860.0410.08510.0012128413129720131727
    3793740.13540.21760.00222.4760.0500.08250.0014126913126526125832
    43108400.58690.32910.00325.0840.0680.11210.0013183418183425183321
    51333720.39410.33460.00335.2470.0710.11370.0014186118186025186022
    6327030.45270.04290.00040.3080.00650.05210.00102713273628946
    71434120.23190.33650.00335.2920.0720.11410.0014187018186825186522
    81353820.24960.33960.00335.3390.0740.11400.0014188518187526186522
    938410920.05950.35530.00355.9410.0820.12130.0015196019196727197522
    10153230.50970.04360.00040.3090.00810.05150.00132753274726258
    11692820.33320.23320.00232.7770.0380.08640.0011135113134919134724
    121715360.15160.31730.00344.8820.0700.11160.0013177719179926182521
    13605620.27320.10960.00161.2100.0240.08010.00126701080516119830
    141965940.17590.32110.00325.2760.0720.11920.0014179518186525194421
    151293360.30510.35560.00356.1210.0850.12480.0016196119199328202722
    16255450.58420.04290.00040.3050.00630.05160.00102713271626745
    17832360.42690.32470.00325.1220.0710.11440.0014181218184026187122
    183148280.51670.33730.00335.4800.0750.11780.0014187418189726192322
    191524140.53780.32350.00325.2570.0710.11790.0014180718186225192421
    样品号14ELT3
    201284950.34990.23780.00313.5630.0610.10870.0013137518154126177822
    211584900.20360.31660.00314.8950.0660.11220.0013177318180124183521
    2254911.28760.44130.00499.7250.150.15980.0020235726240936245421
    233159310.16020.33540.00335.2730.0720.11400.0014186418186425186422
    24572470.30080.22540.00222.6200.0380.08430.0011131013130619129925
    25316680.64370.04320.00040.31100.00600.05220.00092733275529441
    262346970.08920.33970.00355.4630.0780.11660.0014188519189527190522
    271153420.19640.33270.00335.2910.0710.11530.0014185218186725188521
    282627600.11220.34650.00345.7190.0770.11970.0014191819193426195221
    29472110.27150.22120.00222.5970.0370.08510.0011128813130019131925
    302748110.18060.33610.00335.3020.0720.11440.0014186819186925187021
    31671950.43720.32180.00325.3040.0740.11950.0015179818186926194922
    321265520.35280.22440.00222.6550.0370.08580.0011130513131618133424
    33862930.40510.27820.00273.9860.0560.10390.0013158316163123169523
    342397320.10510.33020.00325.2090.0710.11440.0014183918185425187122
    351143130.82600.31730.00314.9560.0670.11330.0014177617181225185322
    36892780.27110.31320.00314.8500.0680.11230.0014175718179425183722
    37431220.51460.32770.00325.2430.0740.11600.0015182718186026189622
    38341330.85330.22330.00222.6150.0410.08490.0012129913130520131428
    39275930.53040.04320.00040.31240.00650.05250.00102723276630845
    40245210.54000.04320.00040.31240.00730.05240.00122733276630451
    41572450.44160.21930.00212.5450.0360.08420.0011127812128518129725
    42641640.77680.33570.00335.4270.0800.11730.0015186618188928191524
    433119300.19760.32950.00325.0930.0680.11210.0013183618183525183421
    441255410.25670.22900.00232.7110.0370.08590.0010132913133118133523
    451273160.74510.34200.00345.5650.0750.11800.0014189619191126192721
    463038790.06480.34590.00336.1270.0830.12850.0015191518199427207721
    471646280.16750.25970.00253.7340.0500.10430.0013148814157921170222
    48713180.13460.22570.00222.7500.0390.08840.0011131213134219139024
    491043840.27920.25810.00263.6200.0500.10170.0012148015155422165623
    502069140.36040.21300.00283.2620.0510.11110.0014124516147223181722
    51132550.68050.04300.00040.30810.0110.05190.00172723273928376
    52962520.49240.33810.00335.4680.0740.11730.0014187818189625191521
    531573400.17160.43640.00429.5400.130.15860.0019233423239132244020
    541375660.38660.22590.00222.7080.0370.08690.0010131313133118135923
    55974030.25340.23310.00242.8470.0400.08860.0011135114136819139523
    561976520.29750.27910.00294.5710.0680.11880.0015158716174426193823
    571363520.57260.32460.00325.7340.0790.12810.0016181218193627207221
    587913860.14930.05920.00060.44420.00690.05450.00083714373639032
    59143150.39660.04300.00040.30910.00960.05220.00162713274829369
    603058310.03440.36280.00377.6380.110.15270.0018199621218930237620
    样品号14ELT3
    612045430.55560.33720.00345.4100.0730.11640.0014187319188626190121
    62994530.21330.22150.00222.5960.0360.08500.0010129013130018131623
    631799100.22860.19590.00282.3640.0390.08750.0010115317123220137223
    641426510.17980.22220.00232.6200.0360.08550.0010129413130618132723
    653068330.63490.33390.00345.2240.0700.11350.0013185719185725185621
    662767980.32710.33370.00335.2700.0700.11450.0013185618186425187321
    671687300.34640.22680.00232.6820.0360.08580.0010131813132418133322
    681064660.26130.22770.00232.6910.0370.08570.0010132213132618133223
    692236300.21500.34580.00355.7590.0790.12080.0014191519194026196821
    702229930.16730.22840.00222.6880.0360.08540.0010132613132518132423
     注:灰色阴影部分为不和谐数据
    下载: 导出CSV

    表 2  三面井组和额里图组砂岩碎屑锆石Lu-Hf 同位素组成

    Table 2.  Lu-Hf isotopic compositions of detrital zircons for sandstonesfrom the Sanmianjing Formation and Elitu Formation

    样品号年龄/Ma176Yb/177Hf176Lu/177Hf176Hf/177HfεHf(0)εHf(t)TDM/MaTDM2/MafLu/Hf
    14SMJ4.118720.00760.00020.2815480.000023-43.3-1.923402631-0.99
    14SMJ4.22800.05280.00210.2824440.000024-11.6-5.811791667-0.94
    14SMJ4.318650.00880.00030.2816520.000020-39.61.522052415-0.99
    14SMJ4.425190.03070.00090.2811730.000022-56.5-1.628923113-0.97
    14SMJ4.519540.02660.00080.2816060.000021-41.21.322962500-0.98
    14SMJ4.625160.01170.00040.2811140.000023-58.6-2.929303185-0.99
    14SMJ4.719090.01350.00040.2815270.000022-44.0-2.023762665-0.99
    14SMJ4.820970.03010.00090.2813760.000031-49.4-3.826132920-0.97
    14SMJ4.925360.01590.00050.2811650.000020-56.8-0.928743080-0.98
    14SMJ4.103050.03910.00150.2821110.000021-23.4-17.016302386-0.95
    14SMJ4.1118280.00160.00000.2815160.000016-44.4-3.823722715-1.00
    14SMJ4.123660.02030.00090.2819140.000016-30.4-22.618782778-0.97
    14SMJ4.1318540.01190.00040.2814640.000018-46.3-5.524632838-0.99
    14SMJ4.143690.01670.00070.2818790.000017-31.6-23.719142850-0.98
    14SMJ4.1525130.00900.00040.2811560.000016-57.2-1.528753098-0.99
    14SMJ4.1618840.02430.00090.2815510.000018-43.2-2.323762668-0.97
    14SMJ4.1719540.01050.00040.2814830.000015-45.6-2.524372735-0.99
    14SMJ4.1818990.01320.00050.2815100.000017-44.6-2.924062717-0.99
    14SMJ4.1918760.01760.00060.2815010.000023-45.0-3.924262760-0.98
    14SMJ4.2019060.02410.00070.2815030.000016-44.9-3.324312747-0.98
    14SMJ4.2118990.01610.00050.2814930.000020-45.2-3.624312756-0.98
    14SMJ4.2219190.01220.00040.2813670.000018-49.7-7.425913007-0.99
    14SMJ4.2319340.02830.00090.2815930.000021-41.70.323172546-0.97
    14SMJ4.2425080.03120.00100.2812380.000023-54.30.228132993-0.97
    14SMJ4.2518460.02100.00060.2815380.000021-43.6-3.223742695-0.98
    14SMJ4.2627110.02060.00070.2810520.000017-60.8-1.330393238-0.98
    14SMJ4.2718070.01080.00040.2815090.000023-44.7-4.924022769-0.99
    14SMJ4.2818850.02880.00080.2814870.000026-45.4-4.524602804-0.97
    14SMJ4.2918000.00300.00010.2812970.000015-52.2-12.226673212-1.00
    14SMJ4.3025070.02560.00080.2811600.000024-57.0-2.229023139-0.98
    14ELT3.113070.02930.00100.2817460.000022-36.3-8.221152592-0.97
    14ELT3.212580.03200.00100.2817270.000028-37.0-9.921382660-0.97
    14ELT3.318330.02630.00080.2816960.000025-38.11.821732376-0.98
    14ELT3.42710.04580.00140.2821690.000035-21.3-15.715452276-0.96
    14ELT3.519750.03600.00110.2817050.000026-37.74.821782297-0.97
    14ELT3.62750.04410.00140.2821950.000030-20.4-14.615082215-0.96
    14ELT3.713470.03050.00100.2818400.000024-33.0-4.019832360-0.97
    14ELT3.820270.01920.00060.2815510.000027-43.21.323572557-0.98
    14ELT3.918350.02340.00080.2815740.000019-42.4-2.423362638-0.98
    14ELT3.1024540.01870.00070.2814970.000031-45.18.824352423-0.98
    14ELT3.1112990.04820.00160.2817790.000023-35.1-7.821022557-0.95
    14ELT3.122730.03960.00140.2822710.000022-17.7-12.014002047-0.96
    14ELT3.1318850.02410.00090.2816330.000021-40.30.722602484-0.97
    14ELT3.1419520.03780.00140.2816840.000024-38.53.222252382-0.96
    14ELT3.1513190.04080.00140.2818330.000024-33.2-5.220172416-0.96
    14ELT3.1619490.01630.00070.2815810.000021-42.10.523202545-0.98
    14ELT3.1716950.03010.00110.2817600.000023-35.80.721002338-0.97
    14ELT3.1818530.02610.00090.2814780.000023-45.8-5.724782849-0.97
    14ELT3.192720.03980.00140.2821820.000021-20.9-15.215272246-0.96
    14ELT3.2012970.02440.00090.2819110.000024-30.4-2.418792226-0.97
    14ELT3.2120770.00850.00030.2814680.000024-46.1-0.224502682-0.99
    14ELT3.222720.03840.00120.2823220.000030-15.9-10.213231934-0.96
    14ELT3.2319150.02850.00090.2816960.000030-38.03.521752330-0.97
    14ELT3.2424400.01330.00040.2811900.000022-56.0-2.028333074-0.99
    14ELT3.252710.03360.00110.2824610.000026-11.0-5.311241623-0.97
    14ELT3.263710.01920.00060.2820940.000028-24.0-16.016132371-0.98
    14ELT3.2719680.02300.00080.2814970.000025-45.1-2.324432729-0.98
    14ELT3.2813320.03910.00120.2815110.000027-44.6-16.224533104-0.96
    14ELT3.2919010.03850.00120.2817430.000023-36.44.421322266-0.96
    14ELT3.3018560.01600.00050.2815280.000029-44.0-3.223792701-0.99
    下载: 导出CSV
  • [1]

    Windley B F, Alexeiev D, Xiao W J, et al. Tectonic models for accretion of the Central Asian Orogenic Belt[J]. Journal of Geological Society, London, 2007, 164: 31-47. doi: 10.1144/0016-76492006-022

    [2]

    Tang K D. Tectonic development of Paleozoic foldbelts at the north margin of the Sino-Korean Craton[J]. Tectonics, 1990, 9(2): 249-260. doi: 10.1029/TC009i002p00249

    [3]

    Tong Y, Jahn B M, Wang T, et al. Permian alkaline granites in the Erenhot-Hegenshan belt, northern Inner Mongolia, China: Model of generation, time of emplacement and regional tectonic significance[J]. Journal of Asian Earth Sciences, 2015, 97: 320-336. doi: 10.1016/j.jseaes.2014.10.011

    [4]

    邵济安. 中朝板块北缘中段地壳演化[M]. 北京:北京大学出版社, 1991:1-136.

    [5]

    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.cnki.com.cn/Article/CJFDTOTAL-JDXK199703005.htm

    [6]

    徐备,赵盼,鲍庆中,等. 兴蒙造山带前中生代构造单元划分初探[J]. 岩石学报,2014,30(7):1841-1857. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201407001.htm

    [7]

    邵济安,何国琦,唐克东. 华北北部二叠纪陆壳演化[J]. 岩石学报, 2015,31(1):47-55. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201501003.htm

    [8]

    Wang Q, Liu X Y. Paleoplate tectonics between Cathaysia and Angaraland in Inner Mongolia[J]. Tectonics, 1986, 5(7): 1073-1088. doi: 10.1029/TC005i007p01073

    [9]

    Xiao W J, Windley B F, Hao J, et al. Accertion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt[J]. Tectonics, 2003, 22(6): 1-20.

    [10]

    Xiao W J, Windley B F, Huang B C, et al. End-Permian to mid-Triassic termination of the accretionary processes of the southern Altaids: implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia[J]. International Journal of Earth Sciences, 2009, 98(6): 1189-1217. doi: 10.1007/s00531-008-0407-z

    [11]

    Li J Y. Permian geodynamic setting of Northeast China and adjacent regions: closure of the Paleo-Asian Ocean and subduction of the Paleo-Pacific Plate[J]. Journal of Asian Earth Sciences, 2006, 26: 207-224. doi: 10.1016/j.jseaes.2005.09.001

    [12]

    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的约束[J]. 岩石学报,2007,23(3):565-582. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200703006.htm

    [13]

    石玉若,刘翠,邓晋福,等. 内蒙古中部花岗质岩类年代学格架及该区构造岩浆演化讨论[J]. 岩石学报,2014,30(11):3155-3171. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201411005.htm

    [14]

    Iizuka T, Hirata T. Improvements of precision and accuracy in situ Hf isotope microanalysis of zircon using the laser ablation MCICP MS technique. Chemical Geology, 2005, 220(1): 121-137.

    [15]

    张海华,郑月娟,陈树旺,等. 内蒙古巴林左旗二叠系碎屑锆石LA-ICP-MS U-Pb年龄及构造意义[J]. 地质学报,2015,89(10): 1703-1717. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201510001.htm

    [16]

    郑月娟,公繁浩,陈树旺,等. 内蒙古西乌珠穆沁旗地区下二叠统原寿山沟组碎屑锆石LA-ICP-MS U-Pb年龄及地质意义[J]. 地质通报,2013,32(8):1260-1268. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20130812&journal_id=gbc

    [17]

    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,1991:1-725.

    [18]

    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. https://www.researchgate.net/profile/Shuan-Hong_Zhang/publication/268370946_Origin_and_evolution_of_the_Bainaimiao_arc_belt_Implications_for_crustal_growth_in_the_southern_Central_Asian_orogenic_belt/links/5548413e0cf2b0cf7aceb843.pdf

    [19]

    黄汲清. 中国主要地质构造单元[M]. 北京:地质出版社,1954:1-102.

    [20]

    耿建珍,李怀坤,张健,等. 锆石Hf同位素组成的LA-MC-ICPMS测定[J]. 地质通报,2011,30(10):1508-1514. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20111004&journal_id=gbc

    [21]

    Nowell G M, Kempton P D, Noble S R, et al. High precision Hf isotope measurements of MORB and OIB by thermal ionization mass spectrometry: insights into the depleted mantle[J]. Chemical Geology, 1998, 149(3/4):211-233.

    [22]

    Blichert-Toft J, Albarede F. The Lu-Hf geochemistry of the chondrites and the evolution of the mantle-crust system[J]. Earth and Planetary Science Letters, 1997, 148: 243-258. doi: 10.1016/S0012-821X(97)00040-X

    [23]

    吴元保,郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报,2004,49(16):1589-1604. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200416001.htm

    [24]

    张志存,盛金章. 内蒙古白乃庙Parafusulina动物群[J]. 微体古生物学报,1987,4(3):237-246. http://www.cnki.com.cn/Article/CJFDTOTAL-WSGT198703000.htm

    [25]

    周祖仁. 湘东南早二叠世栖霞中、晚期的staffella vulgaris (sp. nov.),Misellinaclaudiae及Parafusulinamultiseptata 䗴类群[J]. 古生物学报,1984,23(1):107-123.

    [26]

    内蒙古自治区地质矿产局. 内蒙古自治区岩石地层[M]. 武汉:中国地质大学出版社,1996:1-344.

    [27]

    田树刚,李子舜,王峻涛,等. 内蒙古东部及邻区石炭纪-二叠纪构造地层格架与形成环境[J]. 地质通报,2012,31(10):1554-1564. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20121002&journal_id=gbc

    [28]

    Yang J H, Wu F Y, Shao J A, et al. Constraints on the timing of uplift of the Yanshan Fold and Thrust Belt, North China[J]. Earth and Planetary Science Letters, 2006, 246(3/4): 336-352. https://www.researchgate.net/publication/223423132_Constraints_on_the_timing_of_uplift_of_the_Yanshan_Fold_and_Thrust_Belt_North_China

    [29]

    洪大卫,王式广,谢锡林,等. 兴蒙造山带正εNd(t)值花岗岩的成因和大陆地壳生长[J]. 地学前缘,2000,7(2):441-456.

    [30]

    Zhang S H, Zhao Y, Song B, et al. Carboniferous granitic plutons from the northern margin of the North China block: Implications for a late Paleozoic active continental margin[J]. Journal of Geological Society, 2007, 164(2): 451-463. doi: 10.1144/0016-76492005-190

    [31]

    王芳,陈福坤,候振辉,等. 华北陆块北缘崇礼-赤城地区晚古生代花岗岩类的锆石年龄和Sr-Nd-Hf同位素组成[J]. 岩石学报, 2009,25(11):3057-3074. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200911035.htm

    [32]

    Zhang S H, Zhao Y, Santosh M. Mid-Mesoproterozoic bimodal magmatic rocks in the northern North China Craton: Implications for magmatism related to breakup of the Columbia supercontinent[J]. Precambrian Research, 2012, 222/223: 339-367. doi: 10.1016/j.precamres.2011.06.003

    [33]

    Wang Q H, Yang H, Yang D B, et al. Mid-Mesoproterozoic (~ 1.32Ga) diabase swarms from the western Liaoning region in the northern margin of the North China Craton: BaddeleyitePb-Pb geochronology, geochemistry and implications for the final breakup of the Columbia supercontinent[J]. Precambrian Research, 2014, 254: 114-128. doi: 10.1016/j.precamres.2014.08.005

    [34]

    翟明国,卞爱国. 华北克拉通新太古代末超大陆拼合及古元古代末-中元古代裂解[J]. 中国科学(D辑),2000,30(增刊):129-137. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2000S1016.htm

    [35]

    刘树文,吕勇军,凤永刚,等. 冀北单塔子杂岩的地质学和锆石U-Pb年代学[J]. 高校地质学报,2007,13(3):484-497. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200703012.htm

    [36]

    简平,张旗,刘敦一,等. 内蒙古固阳晚太古代赞岐岩(sanukite)——角闪花岗岩的SHRIMP定年及其意义[J]. 岩石学报, 2005,21(1):151-157. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200501016.htm

    [37]

    韩国卿,刘永江,温泉波,等. 西拉木伦河缝合带北侧二叠纪砂岩碎屑锆石LA-ICP-MSU-Pb年代学及其构造意义[J]. 地球科学-中国地质大学学报,2012,36(4):687-702. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201104008.htm

    [38]

    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://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201407007.htm

    [39]

    Li J Y, Guo F, Li C W, et al. Permian back-arc extension in central Inner Mongolia, NE China: Elemental and Sr-Nd-Pb-Hf-O isotopic constraints from the Linxi high-MgOdiabasedikes[J]. Island Arc, 2015, 24: 404-424. doi: 10.1111/iar.2015.24.issue-4

    [40]

    Shi Y R, Anderson J L, Li L L, et al. Zircon ages and Hf isotopic compositions of Permian and Triassic A-type granites from central Inner Mongolia and their significance for late Palaeozoic and early Mesozoic evolution of the Central Asian Orogenic Belt[J]. International Geology Review, 2016, 58(8): 967-982. doi: 10.1080/00206814.2016.1138333

    [41]

    Eizenhöfer P R, Zhao G C, Sun M, et al. Geochronological and Hf isotopic variability of detrital zircon in Paleozoic strata across the accretionary collision zone between the North China craton and Mongolia arcs and tectonic implications[J]. Geological Society of America Bulletin, 2015, 127(9/10): 1422-1436.

    [42]

    Zhao P, Xu B, Tong Q L, et al. Sedimentological and geochronological constraints on the Carboniferous evolution of central Inner Mongolia, southeastern Central Asian Orogenic Belt: Inland sea deposition in a post-orogenic setting[J]. Gondwana Research, 2016, 31: 253-270. doi: 10.1016/j.gr.2015.01.010

    [43]

    王荃,刘雪亚,李锦轶. 中国内蒙古中部的古板块构造[J]. 中国地质科学院院报,1991,第22号: 1-15. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB199101000.htm

    [44]

    马旭,陈斌,陈家富,等. 华北克拉通北缘晚古生代岩体的成因和意义:岩石学、锆石U-Pb年龄、Nd-Sr同位素及锆石原位Hf同位素证据[J]. 中国科学:地球科学,2012,42(12):1830-1850. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201212006.htm

    [45]

    王挽琼,徐仲元,刘正宏,等. 华北板块北缘中段早中二叠世的构造属性:来自花岗岩类锆石U-Pb年代学及地球化学的制约[J]. 岩石学报,2013,29(9):2987-3003. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201309003.htm

    [46]

    Li Y L, Zhou H W, Brouwer, F M, et al. Late Carboniferous-Middle Permian arc/forearc-related basin in Central Asian Orogenic Belt: Insights from the petrology and geochemistry of the Shuangjing Schist in Inner Mongolia, China[J]. Island Arc, 2011, 20: 535-549. doi: 10.1111/j.1440-1738.2011.00784.x

    [47]

    Zhang X H, Mao Q, Zhang H F, et al. Mafic and felsic magma interaction during the construction of high-K calc-alkaline plutons within a metacratonic passive margin: The early Permian Guyang batholith from the northern North China Craton[J]. Lithos, 2011, 125: 569-591. doi: 10.1016/j.lithos.2011.03.008

    [48]

    Zhang Z, Zhang H F, Shao J A, et al. Mantle upwelling during Permian to Triassic in the northern margin of the North China Craton: Constraints from southern Inner Mongolia[J]. Journal of Asian Earth Sciences, 2014, 79: 112-129. doi: 10.1016/j.jseaes.2013.09.015

    [49]

    李洪颜,徐义刚,黄小龙,等. 华北克拉通北缘晚古生代活化:山西宁武-静乐盆地上石炭统太原组碎屑锆石U-Pb测年及Hf同位素证据[J]. 科学通报,2009,54(5):632-640. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200905017.htm

    [50]

    Wang Y, Zhou L Y, Zhao L J. Cratonic reactivation and orogeny: An example from the northern margin of the North China Craton[J]. Gondwana Research, 2013, 24: 1203-1222. doi: 10.1016/j.gr.2013.02.011

    [51]

    Cawood P A, Hawkesworth C J, Dhuime B. Detrital zircon record and tectonic setting[J]. Geology, 2012, 40(10): 875-878. doi: 10.1130/G32945.1

    [52]

    Chen Y, Zhang Z C, Li K, et al. Detrital zircon U-Pb ages and Hf isotopes of Permo-Carboniferous sandstones in central Inner Mongolia, China: Implications for provenance and tectonic evolution of the southeastern Central Asian Orogenic Belt[J]. Tectonophysics, 2016, 671: 183-201. doi: 10.1016/j.tecto.2016.01.018

    [53]

    Luo Z W, Zhang Z C, Li K, et al. Petrography, geochemistry, and U-Pb detrital zircon dating of early Permian sedimentary rocks from the North Flank of the North China Craton: Implications for the late Palaeozoic tectonic evolution of the eastern Central Asian Orogenic Belt[J]. International Geology Review, 2016, 58(7): 787-806. doi: 10.1080/00206814.2015.1118646

    [54]

    Wang Y, Luo Z H, Santosh M, et al. The Liuyuan volcanic belt in NW China revisited: Evidence for Permian rifting associated with the assembly of continental blocks in the Central Asian Orogenic Belt[J]. Geological Magazine, 2016, 1: 1-21. https://www.researchgate.net/publication/293017274_The_Liuyuan_Volcanic_Belt_in_NW_China_revisited_evidence_for_Permian_rifting_associated_with_the_assembly_of_continental_blocks_in_the_Central_Asian_Orogenic_Belt

    [55]

    张晓晖,翟明国. 华北北部古生代大陆地壳增生过程中的岩浆作用与成矿效应[J]. 岩石学报,2010,26(5):1329-1341. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201005001.htm

    [56]

    Yarmolyuk V V, Kovalenko V I, Kozlovsky A M, et al. Late Paleozoic-Early Mesozoic rift system of Central Asia: composition of magmatic rocks, sources, order of formation and geodynamics[C]// Kovalenko V I. Tectonic problems of Central Asia. World of Science Publisher, Moscow, 2005: 197-226.

    [57]

    Yarmolyuk V V, Kovalenko V I,Kozlovsky A M, et al. Crust-forming processes in the Hercynides of the Central Asian Foldbelt[J]. Petrology, 2008, 16: 679-709. doi: 10.1134/S0869591108070035

    [58]

    Blight J H S, Crowley Q G, Petterson M G, et al. Granites of the southern Mongolia Carboniferous arc: New geochronological and geochemical constraints[J]. Lithos, 2010, 116: 35-52. doi: 10.1016/j.lithos.2010.01.001

    [59]

    洪大卫,黄怀曾,肖宜君,等. 内蒙古中部二叠纪碱性花岗岩及其地球动力学意义[J]. 地质学报,1994,68(3):219-230. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199403002.htm

    [60]

    陈彦,张志诚,李可,等. 内蒙古西乌旗地区二叠纪双峰式火山岩的年代学、地球化学特征和地质意义[J]. 北京大学学报(自然科学版),2014,50(5):843-858. http://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ201405008.htm

    [61]

    徐佳佳,赖勇,崔栋,等. 内蒙古前进场岩体岩石学与锆石U-Pb年代学研究[J]. 北京大学学报(自然科学版),2012,48(4):617-628. http://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ201204011.htm

    [62]

    施光海,苗来成,张福勤,等. 内蒙古锡林浩特A型花岗岩的时代及区域构造意义[J]. 科学通报,2004,49(4):384-389. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200404015.htm

    [63]

    Chen C, Zhang Z C, Li K, et al. Geochronology, geochemistry, and its geological significance of the Damaoqi Permian volcanic sequences on the northern margin of the North China Block[J]. Journal of Asian Earth Sciences, 2015, 97: 307-319. doi: 10.1016/j.jseaes.2014.06.024

    [64]

    蒋孝君,刘正宏,徐仲元,等. 内蒙古镶黄旗乌兰哈达中二叠世碱长花岗岩LA-ICP-MS锆石U-Pb年龄和地球化学特征[J]. 地质通报,2013,32(11):1760-1768. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20131108&journal_id=gbc

  • 加载中

(6)

(2)

计量
  • 文章访问数:  396
  • PDF下载数:  4
  • 施引文献:  0
出版历程
收稿日期:  2016-11-14
修回日期:  2017-01-24
刊出日期:  2017-03-25

目录