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    内蒙古西乌旗南部晚古生代侵入岩年代学、地球化学特征及地质意义

    刘敏 赵洪涛 张达 熊光强 狄永军

    刘敏, 赵洪涛, 张达, 熊光强, 狄永军, 2017. 内蒙古西乌旗南部晚古生代侵入岩年代学、地球化学特征及地质意义. 地球科学, 42(4): 527-548. doi: 10.3799/dqkx.2017.042
    引用本文: 刘敏, 赵洪涛, 张达, 熊光强, 狄永军, 2017. 内蒙古西乌旗南部晚古生代侵入岩年代学、地球化学特征及地质意义. 地球科学, 42(4): 527-548. doi: 10.3799/dqkx.2017.042
    Liu Min, Zhao Hongtao, Zhang Da, Xiong Guangqiang, Di Yongjun, 2017. Chronology, Geochemistry and Tectonic Implications of Late Palaeozoic Intrusions from South of Xiwuqi, Inner Mongolia. Earth Science, 42(4): 527-548. doi: 10.3799/dqkx.2017.042
    Citation: Liu Min, Zhao Hongtao, Zhang Da, Xiong Guangqiang, Di Yongjun, 2017. Chronology, Geochemistry and Tectonic Implications of Late Palaeozoic Intrusions from South of Xiwuqi, Inner Mongolia. Earth Science, 42(4): 527-548. doi: 10.3799/dqkx.2017.042

    内蒙古西乌旗南部晚古生代侵入岩年代学、地球化学特征及地质意义

    doi: 10.3799/dqkx.2017.042
    基金项目: 

    中国地质调查局地质调查项目 1212011085490

    详细信息
      作者简介:

      刘敏 (1991-),男,博士研究生,主要从事矿物学、岩石学、矿床学专业研究.ORCID:0000-0002-9784-9996.E-mail: liumin6364@163.com

      通讯作者:

      张达,ORCID:0000-0001-7145-8850.E-mail: zhangda@cugb.edu.cn

    • 中图分类号: P581

    Chronology, Geochemistry and Tectonic Implications of Late Palaeozoic Intrusions from South of Xiwuqi, Inner Mongolia

    • 摘要: 为探讨兴蒙造山带南蒙古陆块南缘晚古生代的构造演化,对出露于西乌旗南部石英闪长岩、花岗闪长岩和黑云母花岗岩开展了详细的年代学、岩石地球化学及Hf同位素特征研究.结果表明:石英闪长岩、花岗闪长岩和黑云母花岗岩分别形成于330±2 Ma、274±1 Ma及271±1 Ma~282±1 Ma.石英闪长岩属高镁闪长岩/安山岩类 (HMA),与俯冲洋壳板片上部地幔楔中地幔橄榄岩的熔融作用有关,而花岗闪长岩及黑云母花岗岩的源区可能与新生地壳的部分熔融有关.结合区域成果,推测西乌旗南部晚古生代侵入岩均形成于古亚洲洋向北侧南蒙古陆块持续俯冲的阶段,早石炭世石英闪长岩属活动大陆边缘弧岩浆活动,早二叠世花岗闪长岩和黑云母花岗岩则是俯冲过程中短暂弧后伸展阶段的产物.

       

    • 图  1  研究区地质简图

      a.内蒙古中部构造格局示意图,据Jian et al.(2008)及索伦山-锡林郭勒1:50万区域地质图改编;b.西乌旗南部达青牧场地区地质简图,据内蒙古西乌珠穆沁旗幅1:20万地质图改编

      Fig.  1.  Geological sketch of research area

      图  2  研究区典型矿物样品的显微镜下 (正交偏光) 照片

      石英闪长岩 (a, P01)、花岗闪长岩 (b, XW01) 及黑云母花岗岩 (c, XW03; d, XW09)

      Fig.  2.  Photomicrographs (crossed nicols) of the typical mineral samples in research area

      图  3  石英闪长岩 (a)、花岗闪长岩 (b) 及黑云母花岗岩 (c, d) 锆石阴极发光图像

      Fig.  3.  CL images of zircons of quartz diorite (a), granodiorite (b) and biotite granite (c, d)

      图  4  研究区石英闪长岩 (P01-b6)、花岗闪长岩 (XW01-b7) 及黑云母花岗岩 (XW03-b7、XW09-b6) 锆石U-Pb年龄谐和图和加权年龄平均值

      Fig.  4.  Zircon U-Pb concordia diagrams and histograms for the investigated intrusions, P01-b6, quartz diorite; XW01-b7, granodiorite; XW03-b7 and XW09-b6, biotite granite

      图  5  石英闪长岩εHf(t)-年龄图解

      图a中East Xing-Meng及Yanshan Belt背景值据Chen et al.(2009)Xiao et al.(2004)Yang et al.(2006);图b中背景值据Chen et al.(2009)Liu et al.(2009)Liu et al.(2011, 2013)、Hu et al.(2015)Li et al.(2015b)周文孝 (2012)Shi et al.(2016)

      Fig.  5.  Plot of zircon εHf(t) values vs. 206Pb/238U age for the studied quartz diorite

      图  6  研究区侵入岩TAS图解

      Middlemost et al.(1994)Irvine and Baragar (1971)

      Fig.  6.  TAS diagram for the intrusions from our study area

      图  7  研究区侵入岩SiO2-K2O图解及A/CNK-A/NK图解

      a.据Rickwood (1989);b.据Frost et al.(2001);c.据Peccerillo and Taylor (1976)

      Fig.  7.  K2O vs. SiO2 diagram (a), modified alkali-lime index diagram (b) and A/NK vs. A/CNK diagram (c) for the studied intrusions

      图  8  球粒陨石标准化REE图解及微量元素原始地幔标准化图解

      a.据Boynton (1984)Sun和Mcdonough (1989);b.据Sun和Mcdonough (1989)

      Fig.  8.  Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element patterns (b)

      图  9  石英闪长岩Sm/Th-Th/Y图解 (a)、La/Nb-La/Ba图解 (b)、Th/Yb-Sr/La图解 (c) 及Th/Nb-Ba/Th图解 (d)

      邓晋福等 (2010);CLM.大陆岩石圈地幔

      Fig.  9.  Sm/Th-Th/Y (a), La/Nb-La/Ba (b), Th/Yb-Sr/La (c) and Th/Nb-Ba/Th (d) diagrams for the studied quartz diorite

      图  10  HMA SiO2-MgO图解及FeOT/MgO-SiO2图解

      PQ及PS线分别为HMA与MA、MA与非MA分界线;HT.高温;MT.中温;LT.低温;LF.低铁;据Elliott et al.(1997)

      Fig.  10.  SiO2-MgO and FeOT/MgO-SiO2 diagrams for HMA

      图  11  研究区侵入岩F-An-Or三角相图

      Castro (2013);a.同化混染;b.残余体不混融

      Fig.  11.  F-An-Or pseudo-ternary diagram for the studied intrusions

      表  1  内蒙古西乌旗地区南部侵入岩锆石U-Pb数据

      Table  1.   U-Pb isotopic compositions of intrusions from the south of Xiwuqi, Inner Mongolia

      样号及测点 含量 (10-6) 同位素比值 年龄 (Ma)
      Pb U 206Pb/238U 1σ 207Pb/235U 1σ 207Pb/206Pb 1σ 206Pb/238U 1σ 207Pb/235U 1σ 207Pb/206Pb 1σ
      P01-b6-1 791 1 780 0.052 2 0.001 1 0.394 4 0.018 4 0.054 8 0.002 4 328 7 338 13 467 98
      P01-b6-2 120 657 0.052 9 0.001 3 0.411 1 0.025 4 0.059 4 0.003 9 332 8 350 18 589 143
      P01-b6-3 765 1 989 0.052 3 0.001 1 0.393 7 0.018 0 0.054 1 0.002 3 329 7 337 13 376 98
      P01-b6-4 305 1 366 0.052 5 0.001 3 0.410 0 0.021 8 0.056 8 0.002 8 330 8 349 16 483 109
      P01-b6-5 149 686 0.052 4 0.001 3 0.431 2 0.029 9 0.060 5 0.004 1 330 8 364 21 620 142
      P01-b6-6 120 628 0.052 8 0.001 0 0.426 7 0.024 8 0.059 9 0.003 6 331 6 361 18 611 131
      P01-b6-7 685 1 369 0.052 2 0.000 9 0.387 3 0.022 2 0.054 5 0.003 1 328 6 332 16 391 134
      P01-b6-8 199 779 0.052 5 0.001 0 0.403 4 0.023 5 0.055 7 0.003 1 330 6 344 17 439 129
      P01-b6-9 352 1 150 0.052 5 0.000 8 0.405 7 0.019 3 0.056 8 0.002 8 330 5 346 14 483 111
      P01-b6-10 105 574 0.053 5 0.001 0 0.440 8 0.024 8 0.060 5 0.003 3 336 6 371 17 620 125
      P01-b6-11 353 932 0.053 3 0.001 1 0.399 8 0.022 5 0.056 8 0.003 5 335 7 342 16 487 137
      P01-b6-12 369 1 596 0.053 4 0.000 8 0.399 3 0.020 3 0.055 5 0.003 1 335 5 341 15 432 126
      P01-b6-13 301 1 058 0.052 1 0.000 8 0.364 6 0.019 9 0.051 0 0.002 8 327 5 316 15 243 128
      P01-b6-14 66 318 0.054 1 0.001 2 0.477 1 0.037 1 0.067 0 0.005 3 340 7 396 26 839 165
      P01-b6-15 172 634 0.052 3 0.000 9 0.428 3 0.023 5 0.059 4 0.003 4 329 6 362 17 583 124
      P01-b6-16 132 504 0.051 9 0.001 3 0.439 0 0.031 3 0.062 4 0.004 4 326 8 370 22 700 154
      P01-b6-17 101 539 0.052 4 0.001 0 0.379 4 0.022 6 0.052 5 0.003 1 329 6 327 17 309 133
      P01-b6-18 470 1 457 0.051 7 0.000 8 0.356 3 0.015 6 0.049 7 0.002 2 325 5 309 12 183 102
      P01-b6-19 536 1 162 0.052 0 0.001 2 0.394 4 0.031 7 0.055 2 0.004 5 327 7 338 23 420 181
      XW01-b7-1 23 441 0.043 2 0.000 3 0.497 6 0.015 8 0.083 5 0.002 5 273 2 410 13 1 280 58
      XW01-b7-2 22 444 0.043 3 0.000 3 0.470 1 0.015 3 0.078 7 0.002 5 273 2 391 13 1 165 63
      XW01-b7-3 16 349 0.043 3 0.000 3 0.430 4 0.025 6 0.072 1 0.004 1 273 2 363 22 988 117
      XW01-b7-4 26 557 0.043 3 0.000 3 0.571 2 0.018 6 0.095 8 0.002 9 273 2 459 15 1 543 58
      XW01-b7-5 18 396 0.043 4 0.000 3 0.309 4 0.011 7 0.051 7 0.001 9 274 2 274 10 271 85
      XW01-b7-6 32 676 0.043 3 0.000 2 0.434 9 0.013 9 0.072 9 0.002 3 273 2 367 12 1 010 65
      XW01-b7-7 30 605 0.043 2 0.000 3 0.441 6 0.014 5 0.074 2 0.002 4 273 2 371 12 1 046 64
      XW01-b7-8 21 327 0.050 9 0.000 3 0.705 6 0.017 7 0.100 5 0.002 5 320 2 542 14 1 634 46
      XW01-b7-9 31 625 0.043 3 0.000 3 0.547 0 0.019 4 0.091 6 0.003 1 273 2 443 16 1 459 65
      XW01-b7-10 18 398 0.043 2 0.000 2 0.308 6 0.011 0 0.051 8 0.001 8 273 2 273 10 277 80
      XW01-b7-11 20 323 0.053 5 0.000 4 0.653 2 0.021 4 0.088 5 0.002 8 336 2 510 17 1 394 60
      XW01-b7-12 14 309 0.043 2 0.000 3 0.418 7 0.038 8 0.070 3 0.006 5 273 2 355 33 937 190
      XW01-b7-13 17 365 0.043 4 0.000 3 0.308 7 0.012 8 0.051 6 0.002 1 274 2 273 11 268 92
      XW01-b7-14 24 456 0.047 6 0.000 3 0.485 7 0.015 7 0.073 9 0.002 4 300 2 402 13 1 040 64
      XW01-b7-15 22 456 0.043 2 0.000 3 0.406 4 0.015 3 0.068 2 0.002 6 273 2 346 13 874 78
      XW01-b7-16 17 364 0.043 6 0.000 3 0.309 6 0.017 9 0.051 5 0.002 9 275 2 274 16 265 129
      XW01-b7-17 32 739 0.043 3 0.000 3 0.308 8 0.007 2 0.051 7 0.001 2 273 2 273 6 273 51
      XW01-b7-18 18 404 0.043 4 0.000 3 0.308 9 0.016 0 0.051 6 0.002 7 274 2 273 14 268 118
      XW01-b7-19 23 502 0.043 6 0.000 3 0.308 8 0.018 9 0.051 3 0.003 1 275 2 273 17 255 139
      XW01-b7-20 18 415 0.043 2 0.000 3 0.308 5 0.017 0 0.051 8 0.002 8 273 2 273 15 275 123
      XW01-b7-21 28 623 0.043 4 0.000 3 0.308 9 0.009 9 0.051 6 0.001 6 274 2 273 9 268 72
      XW03-b7-1 15 305 0.044 5 0.000 3 0.318 6 0.019 4 0.051 9 0.003 1 281 2 281 17 281 137
      XW03-b7-2 11 215 0.044 5 0.000 3 0.514 5 0.021 3 0.083 8 0.003 4 281 2 421 17 1 289 79
      XW03-b7-3 19 397 0.044 5 0.000 3 0.459 7 0.016 8 0.074 9 0.002 7 281 2 384 14 1 066 72
      XW03-b7-4 18 411 0.044 6 0.000 3 0.322 8 0.021 3 0.052 4 0.003 4 282 2 284 19 305 149
      XW03-b7-5 10 227 0.044 5 0.000 3 0.320 8 0.015 1 0.052 3 0.002 4 281 2 283 13 298 106
      XW03-b7-6 14 310 0.044 6 0.000 3 0.321 7 0.014 6 0.052 3 0.002 4 281 2 283 13 299 103
      XW03-b7-7 13 290 0.044 6 0.000 3 0.319 6 0.013 1 0.052 0 0.002 1 281 2 282 12 284 93
      XW03-b7-8 20 427 0.044 7 0.000 3 0.324 5 0.010 1 0.052 7 0.001 6 282 2 285 9 316 70
      XW03-b7-9 14 304 0.044 8 0.000 4 0.319 5 0.010 1 0.051 7 0.001 7 283 2 282 9 273 75
      XW03-b7-10 22 467 0.044 6 0.000 3 0.500 2 0.021 8 0.081 3 0.003 4 281 2 412 18 1 229 83
      XW03-b7-11 15 329 0.044 7 0.000 3 0.320 2 0.012 1 0.051 9 0.001 9 282 2 282 11 282 85
      XW03-b7-12 17 362 0.044 5 0.000 3 0.504 8 0.021 0 0.082 2 0.003 3 281 2 415 17 1 251 78
      XW03-b7-13 17 339 0.047 9 0.000 3 0.492 3 0.016 5 0.074 5 0.002 4 302 2 406 14 1 054 65
      XW03-b7-14 12 252 0.047 0 0.000 3 0.509 8 0.028 7 0.078 6 0.004 3 296 2 418 24 1 162 108
      XW03-b7-15 23 542 0.044 9 0.000 3 0.321 6 0.009 1 0.052 0 0.001 4 283 2 283 8 285 62
      XW03-b7-16 23 475 0.044 6 0.000 3 0.479 0 0.018 4 0.078 0 0.002 9 281 2 397 15 1 146 75
      XW03-b7-17 27 551 0.044 5 0.000 3 0.540 5 0.013 5 0.088 1 0.002 1 281 2 439 11 1 385 47
      XW03-b7-18 22 495 0.044 8 0.000 3 0.320 6 0.010 9 0.051 9 0.001 7 283 2 282 10 279 75
      XW03-b7-19 22 464 0.044 6 0.000 3 0.407 1 0.020 0 0.066 3 0.003 3 281 2 347 17 814 104
      XW03-b7-20 67 787 0.044 4 0.000 3 0.549 9 0.019 3 0.089 8 0.003 0 280 2 445 16 1 420 65
      XW09-b6-1 36 816 0.042 9 0.000 4 0.306 5 0.009 2 0.051 8 0.001 6 271 2 271 8 276 71
      XW09-b6-2 30 684 0.042 8 0.000 4 0.461 4 0.018 6 0.078 2 0.003 3 270 2 385 15 1 152 84
      XW09-b6-3 34 790 0.042 9 0.000 3 0.304 5 0.008 4 0.051 4 0.001 4 271 2 270 7 260 62
      XW09-b6-4 28 674 0.042 9 0.000 3 0.306 0 0.007 4 0.051 8 0.001 2 270 2 271 7 276 55
      XW09-b6-5 45 1 026 0.042 8 0.000 3 0.399 1 0.009 1 0.067 6 0.001 6 270 2 341 8 857 49
      XW09-b6-6 34 788 0.042 8 0.000 3 0.392 2 0.008 9 0.066 5 0.001 5 270 2 336 8 822 47
      XW09-b6-7 42 924 0.042 8 0.000 3 0.481 9 0.020 6 0.081 7 0.003 3 270 2 399 17 1 237 80
      XW09-b6-8 62 1 447 0.042 4 0.000 3 0.361 2 0.012 4 0.061 7 0.002 0 268 2 313 11 664 69
      XW09-b6-9 53 1 169 0.042 9 0.000 3 0.397 3 0.009 8 0.067 1 0.001 6 271 2 340 8 842 49
      XW09-b6-10 56 1 240 0.042 9 0.000 3 0.364 3 0.008 0 0.061 6 0.001 3 271 2 315 7 660 45
      XW09-b6-11 52 1 212 0.042 8 0.000 3 0.356 7 0.007 8 0.060 4 0.001 3 270 2 310 7 618 45
      XW09-b6-12 33 798 0.043 1 0.000 3 0.307 1 0.017 4 0.051 7 0.002 9 272 2 272 15 273 129
      XW09-b6-13 36 807 0.042 8 0.000 3 0.305 1 0.013 0 0.051 7 0.002 2 270 2 270 12 272 97
      XW09-b6-14 36 804 0.042 8 0.000 3 0.450 9 0.013 9 0.076 4 0.002 3 270 2 378 12 1 105 60
      XW09-b6-15 57 1 230 0.043 2 0.000 3 0.305 7 0.006 2 0.051 3 0.001 0 273 2 271 6 256 46
      XW09-b6-16 47 899 0.048 7 0.000 3 0.491 3 0.010 0 0.073 1 0.001 5 307 2 406 8 1 017 41
      XW09-b6-17 63 1 390 0.043 1 0.000 3 0.304 7 0.007 7 0.051 2 0.001 3 272 2 270 7 252 56
      XW09-b6-18 45 1 003 0.042 9 0.000 3 0.306 5 0.011 5 0.051 8 0.001 9 271 2 271 10 275 84
      XW09-b6-19 34 699 0.046 0 0.000 3 0.485 1 0.015 3 0.076 5 0.002 3 290 2 402 13 1 109 61
      XW09-b6-20 44 1 067 0.042 9 0.000 3 0.306 0 0.005 8 0.051 7 0.000 9 271 2 271 5 273 42
      下载: 导出CSV

      表  2  内蒙古西乌旗南部石英闪长岩锆石Hf同位素分析结果

      Table  2.   Zircon Hf isotopic compositions of the studied quartz diorite from the south of Xiwuqi, Inner Mongolia

      测点 176Hf/177Hf 1σ 176Lu/177Hf 1σ 176Yb/177Hf 1σ εHf(0) εHf(t) TDM1(Ma) TDM2(Ma) fLu/Hf
      P01-b6-1 0.282 908 0.000 025 0.002 796 0.000 071 0.082 085 0.001 746 4.8 11.4 512 572 -0.92
      P01-b6-2 0.282 823 0.000 012 0.000 438 0.000 003 0.011 239 0.000 129 1.8 9.0 599 711 -0.99
      P01-b6-3 0.282 898 0.000 013 0.001 685 0.000 049 0.051 237 0.001 734 4.5 11.3 511 579 -0.95
      P01-b6-4 0.282 782 0.000 011 0.000 622 0.000 001 0.017 449 0.000 109 0.4 7.5 659 794 -0.98
      P01-b6-5 0.282 841 0.000 014 0.000 486 0.000 005 0.012 973 0.000 123 2.4 9.6 575 676 -0.99
      P01-b6-6 0.282 861 0.000 009 0.000 826 0.000 021 0.023 063 0.000 680 3.1 10.2 552 641 -0.98
      P01-b6-7 0.282 897 0.000 017 0.001 315 0.000 042 0.039 303 0.001 404 4.4 11.3 508 576 -0.96
      P01-b6-8 0.282 897 0.000 011 0.000 745 0.000 009 0.020 023 0.000 194 4.4 11.5 500 568 -0.98
      P01-b6-9 0.282 859 0.000 014 0.001 277 0.000 018 0.036 432 0.000 643 3.1 10.1 561 650 -0.96
      P01-b6-10 0.282 862 0.000 011 0.000 493 0.000 004 0.012 579 0.000 075 3.2 10.5 545 632 -0.99
      P01-b6-11 0.282 862 0.000 013 0.000 577 0.000 021 0.015 518 0.000 659 3.2 10.4 547 634 -0.98
      P01-b6-12 0.282 834 0.000 011 0.000 638 0.000 010 0.017 048 0.000 277 2.2 9.4 587 690 -0.98
      P01-b6-13 0.282 852 0.000 010 0.001 001 0.000 018 0.026 683 0.000 416 2.8 9.8 567 661 -0.97
      P01-b6-14 0.282 853 0.000 011 0.000 875 0.000 029 0.023 567 0.000 763 2.9 10.2 563 653 -0.97
      P01-b6-15 0.282 830 0.000 012 0.000 665 0.000 005 0.017 643 0.000 234 2.1 9.1 593 700 -0.98
      P01-b6-16 0.282 866 0.000 012 0.000 845 0.000 017 0.022 197 0.000 535 3.3 10.3 544 632 -0.97
      P01-b6-17 0.282 843 0.000 009 0.000 400 0.000 000 0.009 715 0.000 031 2.5 9.7 571 672 -0.99
      P01-b6-18 0.282 887 0.000 013 0.001 395 0.000 055 0.037 661 0.001 570 4.1 10.9 523 599 -0.96
      P01-b6-19 0.282 886 0.000 016 0.001 314 0.000 015 0.036 360 0.000 526 4.0 10.9 523 599 -0.96
      下载: 导出CSV

      表  3  内蒙古西乌旗地区南部侵入岩主量元素 (%) 分析结果

      Table  3.   Major oxide (%) composition of intrusions from the south of Xiwuqi, Inner Mongolia

      样号 SiO2 TiO2 Al2O3 Fe2O3 FeO MnO MgO CaO Na2O K2O P2O5 LOI Total
      P01-b1 55.05 0.597 13.06 2.52 5.4 0.137 8.53 10.00 1.98 0.841 0.077 1.96 99.30
      P01-b2 54.04 0.551 13.52 2.60 5.5 0.142 8.58 10.14 2.01 1.010 0.075 2.01 99.31
      P01-b3 54.59 0.591 12.96 2.89 5.05 0.138 8.69 10.82 1.83 0.715 0.077 1.86 99.36
      P01-b6 54.16 0.565 13.17 2.87 4.95 0.139 8.62 10.96 2.08 0.723 0.079 1.91 99.39
      XW01-b1 65.97 0.802 16.16 1.31 4.15 0.049 1.36 2.22 3.37 3.620 0.237 0.86 99.52
      XW01-b2 63.62 0.809 16.75 1.94 4.80 0.076 1.96 1.76 3.02 3.620 0.197 1.59 99.42
      XW01-b3 63.52 0.773 16.37 1.73 4.75 0.074 1.91 1.66 2.82 3.670 0.185 2.65 99.41
      XW01-b7 65.43 0.800 16.54 1.48 3.61 0.060 1.55 1.92 3.25 4.170 0.250 0.85 99.06
      XW03-b1 68.74 0.530 15.78 0.72 2.75 0.040 0.92 1.67 3.69 4.150 0.210 0.65 99.20
      XW03-b3 68.69 0.540 15.86 0.73 2.80 0.040 0.93 1.71 3.76 3.940 0.210 0.62 99.21
      XW03-b4 68.93 0.500 15.79 0.88 2.44 0.040 0.87 1.74 3.70 4.140 0.210 0.57 99.24
      XW03-b5 68.18 0.550 15.49 0.89 2.68 0.040 0.92 1.73 3.62 4.130 0.210 0.67 98.44
      XW09-b1 68.06 0.520 15.27 0.64 2.71 0.050 1.44 2.45 3.68 3.140 0.140 1.65 98.10
      XW09-b2 69.17 0.530 15.12 0.45 2.78 0.050 1.40 1.87 3.50 3.500 0.140 1.08 98.51
      XW09-b4 68.14 0.600 15.3 0.61 3.04 0.060 1.60 2.44 3.69 2.940 0.140 1.18 98.56
      XW09-b6 69.59 0.520 15.28 0.64 2.68 0.050 1.40 2.02 3.56 3.330 0.130 1.05 99.20
        Mg#=100×(MgO/40.304)/(MgO/40.304+Fe2O3/159.691×2+FeO/71.846);标准化公式:oxide=(100-total)×oxide/total+oxide (Le Maitre, 2002)(单位:%).
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      表  4  内蒙古西乌旗地区南部侵入岩微量元素 (10-6) 分析结果

      Table  4.   Trace elements (10-6) composition of intrusions from the south of Xiwuqi, Inner Mongolia

      P01-b1 P01-b2 P01-b3 P01-b6 XW01-b1 XW01-b2 XW01-b3 XW01-b7 XW03-b1 XW03-b3 XW03-b4 XW03-b5 XW09-b1 XW09-b2 XW09-b4 XW09-b6
      La 6.10 5.35 5.70 5.30 51.20 41.90 42.00 32.26 37.98 37.40 36.90 33.26 27.63 28.34 28.30 26.26
      Ce 13.10 12.30 12.80 11.80 101.00 82.30 82.30 74.47 85.64 83.12 82.71 75.15 57.28 60.47 59.40 53.51
      Pr 1.79 1.79 1.83 1.70 13.00 10.30 10.20 9.31 10.39 9.97 9.99 9.15 6.79 7.09 7.09 6.80
      Nd 8.05 8.39 8.28 7.80 51.50 39.80 39.50 38.40 43.34 41.84 41.38 38.62 27.57 28.82 29.50 27.88
      Sm 2.04 2.19 2.06 2.00 10.10 7.40 7.32 7.81 8.87 8.45 8.25 7.99 5.47 5.79 5.70 5.84
      Eu 0.64 0.69 0.66 0.63 1.46 1.38 1.35 1.37 1.11 1.05 1.10 0.95 0.92 0.91 0.93 0.96
      Gd 2.26 2.44 2.28 2.30 8.29 6.26 5.89 7.15 8.15 7.65 7.40 7.13 5.14 5.37 5.42 5.62
      Tb 0.47 0.51 0.49 0.48 1.36 1.07 1.02 1.11 1.25 1.16 1.16 1.08 0.87 0.95 0.91 0.96
      Dy 2.74 3.05 2.85 2.78 6.39 5.73 5.13 6.38 6.91 6.25 6.34 6.03 5.07 5.61 5.48 5.96
      Ho 0.55 0.61 0.56 0.55 1.02 0.88 0.82 1.16 1.23 1.07 1.12 1.06 0.96 1.10 1.06 1.15
      Er 1.68 1.85 1.69 1.66 2.70 2.72 2.16 3.28 3.37 2.90 2.98 2.96 2.87 3.17 3.07 3.37
      Tm 0.27 0.31 0.28 0.28 0.41 0.37 0.34 0.48 0.49 0.43 0.43 0.43 0.43 0.50 0.48 0.53
      Yb 1.78 2.01 1.85 1.85 2.54 2.59 2.13 2.89 3.02 2.54 2.77 2.65 2.72 3.22 2.94 3.32
      Lu 0.27 0.31 0.27 0.28 0.35 0.35 0.31 0.46 0.49 0.40 0.43 0.41 0.44 0.52 0.48 0.54
      Y 15.40 17.10 15.70 15.60 28.10 24.40 22.40 31.16 32.37 29.11 29.47 29.50 25.95 28.92 28.18 31.01
      Rb 22.10 30.10 17.00 18.40 114.00 116.00 118.00 130.00 141.00 143.00 142.00 146.00 103.00 111.00 107.00 108.00
      Ba 112.00 154.00 121.00 131.00 1 078.00 941.00 990.00 1 062.00 837.00 755.00 873.00 863.00 525.00 543.00 586.00 598.00
      Hf 1.39 1.44 1.41 1.40 2.12 3.23 2.69 8.82 9.89 10.08 9.25 10.04 7.66 7.10 7.97 6.80
      Ta 0.14 0.14 0.14 0.14 0.69 0.66 0.71 0.90 1.24 1.31 1.06 1.24 0.75 0.89 0.78 0.90
      Pb 3.69 5.12 4.60 3.75 23.70 22.30 22.00 26.04 24.71 24.62 23.30 24.44 18.57 18.59 16.31 20.83
      Th 1.14 0.86 1.42 0.89 17.80 13.50 13.50 11.98 13.77 12.64 11.95 13.41 9.33 9.76 9.25 10.51
      U 0.33 0.31 0.52 0.29 1.69 2.43 2.23 1.62 1.72 1.65 1.59 1.86 1.31 1.40 1.19 2.11
      Nb 1.97 2.00 2.05 1.84 13.70 13.40 14.00 19.29 16.51 17.03 16.29 17.90 12.28 12.10 13.28 12.72
      Sr 232.00 251.00 245.00 230.00 233.00 251.00 263.00 206.00 156.00 158.00 162.00 156.00 136.00 135.00 144.00 131.00
      Zr 30.00 32.40 30.70 32.40 85.00 125.00 103.00 273.00 251.00 260.00 245.00 259.00 179.00 178.00 193.00 170.00
      Cr 544.00 530.00 546.00 535.00 27.30 51.10 49.10 31.30 14.70 16.80 12.70 15.10 30.70 29.00 30.80 30.60
      Ni 113.00 112.00 114.00 116.00 13.00 21.10 19.70 15.14 9.64 9.09 9.46 9.13 14.16 13.66 13.22 14.32
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