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    华北克拉通北缘中段多伦地区早二叠世双峰式岩浆作用

    李天瑜 李世超 李鹏川 彭云彪 那木吉拉 雒德利 赵庆英 孙加鹏

    李天瑜, 李世超, 李鹏川, 彭云彪, 那木吉拉, 雒德利, 赵庆英, 孙加鹏, 2023. 华北克拉通北缘中段多伦地区早二叠世双峰式岩浆作用. 地球科学, 48(8): 2888-2904. doi: 10.3799/dqkx.2021.210
    引用本文: 李天瑜, 李世超, 李鹏川, 彭云彪, 那木吉拉, 雒德利, 赵庆英, 孙加鹏, 2023. 华北克拉通北缘中段多伦地区早二叠世双峰式岩浆作用. 地球科学, 48(8): 2888-2904. doi: 10.3799/dqkx.2021.210
    Li Tianyu, Li Shichao, Li Pengchuan, Peng Yunbiao, Na Mujila, Luo Deli, Zhao Qingying, Sun Jiapeng, 2023. Early Permian Bimodal Magmatism in the Duolun Area of the Central Section of the Northern Margin of the North China Craton. Earth Science, 48(8): 2888-2904. doi: 10.3799/dqkx.2021.210
    Citation: Li Tianyu, Li Shichao, Li Pengchuan, Peng Yunbiao, Na Mujila, Luo Deli, Zhao Qingying, Sun Jiapeng, 2023. Early Permian Bimodal Magmatism in the Duolun Area of the Central Section of the Northern Margin of the North China Craton. Earth Science, 48(8): 2888-2904. doi: 10.3799/dqkx.2021.210

    华北克拉通北缘中段多伦地区早二叠世双峰式岩浆作用

    doi: 10.3799/dqkx.2021.210
    基金项目: 

    国家自然科学基金 41872234

    国家自然科学基金 41872194

    内蒙古自治区地质勘查基金项目 NMKD2015-35

    中国核工业地质局项目 202101

    中国核工业地质局项目 202203-4

    中国核工业地质局项目 202204-1

    详细信息
      作者简介:

      李天瑜(1989-),男,硕士研究生,构造地质学专业. E-mail:tyli18@mails.jlu.edu.cn

      通讯作者:

      李世超, E-mail: lsc@jlu.edu.cn

    • 中图分类号: P597

    Early Permian Bimodal Magmatism in the Duolun Area of the Central Section of the Northern Margin of the North China Craton

    • 摘要: 东大山地区双峰式岩浆岩位于内蒙古多伦县东部,处于华北板块北缘. 岩体由石英二长岩和玄武岩组成. 对其开展了全岩地球化学、锆石U-Pb年代学和Hf同位素组成研究. 研究结果表明:石英二长岩和玄武岩锆石LA-ICP-MS U-Pb定年结果分别为283±1.6 Ma、280±2.9 Ma,形成于早二叠世;二者锆石Hf同位素组成整体较相似,两阶段模式年龄(tDM2)普遍较为古老(1 760~2 354 Ma,仅玄武岩内测得324 Ma、824 Ma两个较新年龄),与华北板块基底接近;岩体SiO2含量在50.64%~65.87%存在明显的间断,具有双峰式岩浆岩特征,都相对富K、Na、Al,亏Ca、Mg,石英二长岩较玄武岩明显亏损Ti、P,具有明显的互补迹象. 结合前人研究成果,认为东大山地区双峰式岩浆岩可能是板块俯冲、后撤引起的伸展背景下,古亚洲洋俯冲板片脱水引起上地幔部分熔融形成的幔源岩浆向上运移、聚集于华北板块之下引起古老基底部分熔融的产物,研究区早二叠世期间构造环境为活动大陆边缘.

       

    • 图  1  研究区大地构造背景(a)及地质简图(b)

      1. 第四系;2. 下白垩统义县组;3. 下白垩统玛尼吐组;4. 下白垩满克头鄂博组;5. 下二叠统额里图组;6. 中元古界白云鄂博群;7. 早白垩世二长花岗岩;8. 早二叠世石英二长岩;9. 采样点

      Fig.  1.  Geological regional location(a) and geological sketch map of research area(b)

      图  2  石英二长岩野外(a)及显微照片(b)、玄武岩野外(c)及显微照片(d)

      Q. 石英;Pl. 斜长石;Or. 正长石;Am. 角闪石

      Fig.  2.  Photographs of field and micro for the quartz monzonite(a, b) and basalt(c, d)

      图  3  石英二长岩、玄武岩锆石CL图像

      白圈代表测试位置,数字代表U-Pb、Lu-Hf测试序号

      Fig.  3.  CL images of quartz monzonite and basalt

      图  4  石英二长岩、玄武岩锆石U-Pb谐和图

      Fig.  4.  U-Pb concordia diagrams of zircon for quartz monzonite and basalt

      图  5  石英二长岩(a)、玄武岩(b)锆石εHf(t)-锆石年龄图解

      Fig.  5.  εHf(t) vs. zircon ages plots for quartz monzonite and basalt

      图  6  石英二长岩TAS图解(a, 据Irvine and Baragar, 1971)和玄武岩Zr/Tio2-Nb/Y图解(b, 据Wilson, 1989

      Fig.  6.  TAS(a, after Irvine and Baragar, 1971) and Zr/Tio2 vs. Nb/Y(b, after Wilson, 1989) classification diagrams for quartz monzonite(a) and basalt(b)

      图  7  石英二长岩、玄武岩稀土元素配分模式图(a, 据Boynton, 1984)和微量元素原始地幔标准化图解(b,据Sun and McDonough,1989

      Fig.  7.  Chondrite-normalized REE pstterns (a, normalization values after Boynton, 1984) and primitive mantle-normalized trace element spider diagrams (b, normalization values after Sun and McDonough, 1989) for quartz monzonite (a) and basalt (b)

      图  8  石英二长岩Ⅰ型-A型花岗岩判别图解(a, 据Collins et al., 1982)和玄武岩La/Yb-Sm/Yb图解(b, 据Xu et al., 2005)

      Fig.  8.  Ⅰ model vs. A model (a, after Collins et al., 1982) and La/Yb vs.Sm/Yb (b, after Xu et al., 2005) classification diagrams for quartz monzonite (a) and basalt (b)

      图  9  东大山地区双峰式岩浆岩Harker图解

      Fig.  9.  Harker diagram of Bimodal magmatites in Duolun area

      图  10  石英二长岩微量元素w(Y+Nb)-w(Rb)构造环境判别图(a,据Pearce et al., 1984)及玄武岩Th-Ta协变判别图解(b, 据Pearce et al., 1982

      ORG. 大洋中脊花岗岩;WPG. 板内花岗岩;VAG. 火山弧花岗岩;Syn-COLG. 同碰撞花岗岩;MORB. 洋中脊玄武岩;WPB. 板内玄武岩;IAB. 岛弧玄武岩;SHO. 橄榄玄武岩;TH. 拉斑玄武岩;TR. 过渡性玄武岩;ALK. 碱性火山弧玄武岩;ICA. 钙碱性玄武岩

      Fig.  10.  w(Y+Nb) vs. w(Rb) (a, after Pearce et al., 1984) and Th vs. Ta (b, after Pearce et al., 1982) classification diagrams for quartz monzonite (a) and basalt (b)

      图  11  东大山地区双峰式岩浆岩形成模型

      据朱日祥和徐日刚(2019)改

      Fig.  11.  Aschematic diagram showing the mechanism in formation of Bimodal magmatites in Duolun area

      表  1  东大山双峰式岩浆岩中的锆石LA-ICP-MS U-Pb定年数据

      Table  1.   LA-ICP-MS zircon U-Pb dating results for quartz monzonite and basalt

      测点 含量 Th/U 同位素比值 年龄
      Th U 206Pb/238U 207Pb/235U 207Pb/206Pb 206Pb/238U 207Pb/235U 207Pb/206Pb
      石英二长岩
      1 135.1 191 0.82 0.044 0.000 6 0.328 0.014 7 0.054 0.002 4 280 4 288 11 369 106
      2 298.5 261 1.26 0.045 0.000 7 0.309 0.013 4 0.051 0.002 2 281 4 274 10 232 102
      3 156.3 236 0.82 0.044 0.000 6 0.325 0.015 4 0.053 0.002 4 279 4 286 12 339 104
      4 210.2 258 0.99 0.044 0.000 6 0.313 0.013 3 0.052 0.002 3 280 4 276 10 333 100
      5 331.4 342 1.31 0.044 0.000 7 0.325 0.012 7 0.053 0.002 0 280 4 285 10 343 90
      6 648.7 763 0.99 0.045 0.000 7 0.351 0.011 5 0.057 0.002 0 281 4 305 9 502 71
      7 203.8 180 1.39 0.046 0.000 8 0.327 0.015 6 0.052 0.002 6 289 5 287 12 295 139
      8 218.3 258 0.94 0.044 0.000 6 0.347 0.016 0 0.057 0.002 7 280 4 302 12 494 106
      9 160.7 206 0.93 0.044 0.000 8 0.344 0.016 5 0.057 0.002 7 280 5 300 12 483 107
      10 416.3 424 1.26 0.044 0.000 8 0.333 0.018 7 0.054 0.003 0 280 5 292 14 383 122
      11 157.1 221 0.97 0.045 0.000 9 0.371 0.024 5 0.060 0.003 7 283 5 320 18 606 140
      12 831.6 408 2.86 0.045 0.000 9 0.303 0.019 3 0.049 0.003 4 285 5 269 15 169 156
      13 681.7 435 1.90 0.045 0.000 6 0.340 0.013 2 0.056 0.002 1 282 4 297 10 435 83
      14 145.6 162 1.05 0.046 0.000 8 0.347 0.016 7 0.055 0.002 6 289 5 302 13 433 104
      15 233.0 232 1.31 0.045 0.000 7 0.316 0.014 7 0.051 0.002 4 286 4 279 11 243 107
      16 148.4 221 0.78 0.044 0.000 8 0.379 0.020 6 0.062 0.003 4 281 5 326 15 700 117
      17 182.3 240 0.93 0.045 0.000 6 0.356 0.013 7 0.058 0.002 3 283 4 309 10 539 92
      18 183.6 268 0.88 0.045 0.000 6 0.311 0.011 4 0.051 0.002 0 286 4 275 9 233 95
      19 148.9 214 0.85 0.046 0.000 7 0.330 0.015 3 0.052 0.002 4 293 4 289 12 272 105
      20 326.3 382 1.06 0.045 0.000 6 0.326 0.012 4 0.052 0.001 9 285 3 286 10 283 83
      21 222.9 242 1.07 0.045 0.000 6 0.363 0.015 6 0.059 0.002 6 282 4 315 12 576 127
      22 220.3 361 0.70 0.046 0.000 6 0.328 0.011 8 0.051 0.001 8 293 4 288 9 261 75
      23 1615 521 3.56 0.044 0.000 6 0.310 0.012 9 0.051 0.002 2 278 4 274 10 256 100
      24 156.6 148 1.31 0.045 0.000 9 0.350 0.022 9 0.057 0.003 8 283 6 305 17 498 148
      25 362.1 504 0.82 0.045 0.000 6 0.323 0.001 0 0.053 0.001 6 282 3 285 8 309 69
      玄武岩
      1 186 256 0.73 0.04 0.000 8 0.34 0.015 0.055 0.002 0 280 5 296 12 433 94
      2 351 292 1.20 0.05 0.000 6 0.36 0.016 0.058 0.003 0 287 4 313 12 522 96
      3 185 250 0.74 0.04 0.000 8 0.32 0.015 0.053 0.003 0 281 5 282 12 309 119
      4 194 272 0.71 0.04 0.000 8 0.36 0.018 0.06 0.003 0 277 5 313 14 611 111
      5 170 177 0.96 0.04 0.001 8 0.33 0.047 0.055 0.009 0 271 11 288 36 432 373
      6* 112 140 0.80 0.04 0.000 9 0.33 0.026 0.064 0.006 0 243 6 286 20 744 198
      7* 788 683 1.15 0.03 0.000 5 0.26 0.008 0.057 0.002 0 207 3 231 6 500 67
      8 290 397 0.73 0.04 0.000 8 0.39 0.015 0.065 0.002 0 277 5 337 11 783 78
      9* 81 107 0.76 0.05 0.000 9 0.58 0.028 0.084 0.004 0 314 5 462 18 1 302 90
      10* 168 248 0.68 0.04 0.000 8 0.33 0.012 0.053 0.002 0 281 5 286 9 324 112
      11 201 364 0.55 0.04 0.000 9 0.32 0.018 0.052 0.003 0 280 5 283 13 306 116
      12* 873 870 1.00 0.03 0.000 5 0.28 0.009 0.061 0.002 0 208 3 248 7 633 59
      13* 1 259 1679 0.75 0.02 0.000 4 0.2 0.006 0.069 0.002 0 135 2 185 5 900 61
      14 319 441 0.72 0.04 0.000 7 0.33 0.012 0.056 0.002 0 274 4 293 9 450 76
      15* 133 198 0.67 0.05 0.000 9 0.37 0.014 0.054 0.002 0 313 6 318 11 391 93
      16* 322 337 0.95 0.04 0.000 8 0.38 0.027 0.072 0.006 0 243 5 324 20 972 159
      17 217 509 0.43 0.04 0.000 6 0.35 0.010 0.059 0.002 0 277 4 308 8 561 64
      注:标*号的数据因不协和而未参加统计
      下载: 导出CSV

      表  2  石英二长岩、玄武岩中锆石的Hf同位素分析结果

      Table  2.   Zircon Hf isotopic data for quartz monzonite and basalt

      测点号 Age(Ma) 176Yb/177Hf 176Lu/177Hf 176Hf/177Hf εHf() εHf(t) TDM TDMc fLu/Hf
      石英二长岩
      1 280 0.037 074 0.000 429 0.001 154 0.000 014 0.282 132 0.000 020 -22.64 -16.70 1 583 2 354 -0.97
      2 281 0.038 734 0.000 140 0.001 201 0.000 004 0.282 202 0.000 024 -20.17 -14.24 1 487 2 198 -0.96
      3 279 0.028 828 0.000 247 0.000 881 0.000 009 0.282 196 0.000 019 -20.37 -14.39 1 482 2 208 -0.97
      4 280 0.054 428 0.000 439 0.001 617 0.000 015 0.282 285 0.000 023 -17.21 -11.34 1 385 2 017 -0.95
      5 280 0.041 198 0.000 270 0.001 215 0.000 008 0.282 253 0.000 020 -18.35 -12.41 1 415 2 084 -0.96
      6 281 0.046 922 0.000 353 0.001 371 0.000 009 0.282 312 0.000 018 -16.28 -10.37 1 339 1 955 -0.96
      7 289 0.044 059 0.001 810 0.001 303 0.000 054 0.282 245 0.000 022 -18.65 -12.54 1 431 2 100 -0.96
      8 280 0.048 764 0.000 347 0.001 487 0.000 015 0.282 311 0.000 020 -16.32 -10.42 1 345 1 960 -0.96
      9 280 0.052 770 0.000 749 0.001 535 0.000 026 0.282 213 0.000 024 -19.76 -13.91 1 484 2 177 -0.95
      10 280 0.048 744 0.000 135 0.001 414 0.000 005 0.282 288 0.000 022 -17.11 -11.21 1 374 2 009 -0.96
      11 283 0.038 939 0.000 132 0.001 153 0.000 002 0.282 290 0.000 023 -17.04 -11.03 1 361 1 999 -0.97
      12 285 0.041 294 0.000 628 0.001 190 0.000 022 0.282 207 0.000 025 -19.98 -13.92 1 479 2 183 -0.96
      13 282 0.058 001 0.000 598 0.001 646 0.000 021 0.282328 0.000 024 -15.69 -9.79 1 325 1 920 -0.95
      14 289 0.046 676 0.000 511 0.001 329 0.000 010 0.282 297 0.000 025 -16.81 -10.74 1 359 1 984 -0.96
      15 286 0.056 501 0.001 133 0.001 579 0.000 032 0.282 239 0.000 025 -18.86 -12.88 1 450 2 117 -0.95
      16 281 0.059 493 0.000 144 0.001 677 0.000 008 0.282 401 0.000 022 -13.11 -7.27 1 223 1 760 -0.95
      17 283 0.034 540 0.000 511 0.000 937 0.000 016 0.282 261 0.000 021 -18.07 -12.03 1 394 2 062 -0.97
      18 286 0.039 795 0.000 275 0.001 110 0.000 005 0.282 197 0.000 024 -20.35 -14.27 1 491 2 207 -0.97
      玄武岩
      1 280 0.051 617 0.000 453 0.001 463 0.000 013 0.282 292 0.000 029 -16.96 -11.08 1 369 1 999 -0.96
      2 287 0.039 388 0.000 622 0.001 058 0.000 016 0.282 282 0.000 024 -17.34 -11.24 1 370 2 015 -0.97
      3 281 0.098 110 0.000 979 0.002 717 0.000 027 0.282 296 0.000 032 -16.84 -11.18 1 412 2 006 -0.92
      4 277 0.043 547 0.000 114 0.001 188 0.000 003 0.282 270 0.000 019 -17.77 -11.87 1 391 2 048 -0.96
      5 271 0.075 961 0.000 978 0.002 194 0.000 033 0.282 222 0.000 026 -19.45 -13.89 1 498 2 170 -0.93
      8 277 0.056 354 0.000 476 0.001 568 0.000 007 0.282 308 0.000 021 -16.42 -10.59 1 352 1 969 -0.95
      10 281 0.045 425 0.000 527 0.001 275 0.000 015 0.282 311 0.000 019 -16.32 -10.38 1 337 1 956 -0.96
      11 280 0.034 278 0.000 075 0.000 988 0.000 004 0.282 814 0.000 019 1.48 7.47 620 824 -0.97
      14 274 0.058 519 0.000 619 0.001 873 0.000 027 0.282 225 0.000 022 -19.34 -13.67 1 481 2 158 -0.94
      17 277 0.051 655 0.000 323 0.001 707 0.000 015 0.283 039 0.000 025 9.44 15.23 307 324 -0.95
      下载: 导出CSV

      表  3  石英二长岩、玄武岩的主量元素(%)、稀土微量元素(×10-6)分析结果表

      Table  3.   Major (%), rare earth and trace element (×10-6)for quartz monzonite and basalt

      样品号 P09-01 P09-03 P09-04 P09-05 P09-06 P13-02 P13-03 P13-04 P13-05
      岩性 石英二长岩 玄武岩
      SiO2 66.37 66.59 66.85 67.17 65.87 50.64 49.31 50.36 48.83
      TiO2 0.33 0.43 0.42 0.35 0.40 3.18 3.18 3.08 3.24
      Al2O3 16.10 16.55 15.89 16.54 16.62 14.63 15.07 14.66 15.81
      Fe2O3 2.77 1.46 1.71 1.37 1.95 9.33 6.65 6.76 6.71
      P2O5 0.12 0.15 0.15 0.12 0.14 0.85 0.88 0.86 0.91
      CaO 1.59 1.84 1.98 1.76 1.85 1.76 2.08 1.81 1.61
      K2O 5.15 4.75 4.72 4.99 4.93 2.68 3.66 3.54 3.92
      MgO 0.62 0.81 0.77 0.68 0.8 4.07 5.02 4.68 5.14
      MnO 0.09 0.09 0.09 0.08 0.08 0.12 0.11 0.12 0.086
      Na2O 4.67 4.72 4.82 4.76 4.9 4.48 2.94 3.45 2.92
      FeO 1.47 1.84 1.81 1.56 1.74 4.35 6.44 6.14 6.48
      LOS 0.37 0.77 0.75 0.65 0.70 3.71 4.25 3.82 3.83
      Total 99.64 100 99.99 100 99.98 99.8 99.59 99.28 99.48
      Mg# 0.23 0.33 0.30 0.32 0.30 0.37 0.43 0.42 0.44
      A/CNK 1.02 1.04 0.97 1.02 1.01 1.28 1.44 1.36 1.61
      AR 3.23 3.11 3.31 3.17 3.26 2.55 2.04 2.44 2.01
      Cr 0.0008 12.8 12.1 13.8 10.8 39.6 27.4 23.8 25.5
      Ni 2.324 4.71 6.5 6.25 5.2 18.7 41.9 17.4 72.4
      Co 3.354 4.28 5.6 3.93 3.97 38.3 42.5 40.4 45.7
      Rb 68.237 69.9 67.2 66.9 66.6 59.8 78.7 72.1 85.7
      Cs 2.949 3.14 2.9 2.72 2.2 1.55 1.26 1.16 1.40
      Sr 323.45 294 319 304 308 181 180 183 164
      Ba 1339.8 1228 1322 1551 1399 1527 2750 2645 2836
      V 0.002 28.7 29.4 26.1 26.5 277 293 272 296
      Sc 4.497 2.98 3.49 2.75 2.46 22.760 3 21.750 9 20.98 22.10
      Nb 8.038 8.75 9.68 7.91 8.13 14.6 14.3 12.8 14.7
      Ta 0.736 1.08 1.43 0.93 0.86 1.64 2.22 2.75 1.53
      Zr 260.25 252 246 241 229 258 226 222 233
      Hf 6.606 1.3 0.5 2.1 1.9 1.20 0.60 0.70 0.50
      U 0.585 0.6 0.62 0.5 0.57 0.93 0.73 0.65 0.68
      Th 12.055 8.46 9.08 7.93 8.58 5.42 3.47 5.02 3.28
      La 66.896 72.676 85.126 59.8 77.342 31.26 26.86 26.41 29.62
      Ce 125.365 129.558 150.264 111.596 140.327 69.75 65.81 60.47 68.21
      Pr 12.16 12.145 14.726 10.867 13.728 10.09 8.96 8.89 10.16
      Nd 36.32 36.513 43.294 32.586 41.365 40.35 39.37 38.11 40.47
      Sm 4.654 4.603 5.27 4.005 4.979 1.2 0.6 0.7 0.5
      Eu 1.067 1.097 1.093 0.913 0.983 2.31 2.33 2.1 2.38
      Gd 4.358 5.848 6.532 4.886 6.244 6.59 6.56 6.33 6.94
      Tb 0.447 0.593 0.626 0.527 0.632 1.2 1.23 1.14 1.26
      Dy 2.267 2.113 2.511 2.063 2.113 6.71 6.81 5.93 7.05
      Ho 0.431 0.372 0.411 0.360 0.376 1.21 1.27 1.12 1.28
      Er 1.172 1.314 1.514 1.211 1.321 3.57 3.62 3.21 3.83
      Tm 0.181 0.163 0.168 0.146 0.151 0.51 0.52 0.49 0.59
      Yb 1.039 1.054 1.168 0.909 1.041 3.17 3.51 3.29 3.73
      Lu 0.159 0.151 0.183 0.142 0.158 0.5 0.52 0.47 0.55
      Y 10.429 10.929 11.449 9.622 10.264 32.99 32 31.48 35.96
      ΣREE 290.7 256.5 268.2 312.9 230.0 185.4 175.66 165.5 184.6
      ΣLREE 278.7 246.5 256.6 299.8 219.8 162.0 151.6 143.5 159.4
      ΣHREE 12.04 10.06 11.61 13.11 10.24 23.44 24.03 21.96 25.22
      LREE/HREE 23.15 24.51 22.11 22.87 21.45 6.91 6.31 6.53 6.32
      δEu 0.54 0.72 0.65 0.57 0.63 0.96 0.97 0.93 0.95
      下载: 导出CSV
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