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    蒙古-鄂霍次克洋的远程作用:来自内蒙古东南部羊盘沟地区流纹斑岩成因的证据

    蒋孝君 彭云彪 董晓杰 李华明 涂颖

    蒋孝君, 彭云彪, 董晓杰, 李华明, 涂颖, 2021. 蒙古-鄂霍次克洋的远程作用:来自内蒙古东南部羊盘沟地区流纹斑岩成因的证据. 地球科学, 46(9): 3057-3073. doi: 10.3799/dqkx.2020.335
    引用本文: 蒋孝君, 彭云彪, 董晓杰, 李华明, 涂颖, 2021. 蒙古-鄂霍次克洋的远程作用:来自内蒙古东南部羊盘沟地区流纹斑岩成因的证据. 地球科学, 46(9): 3057-3073. doi: 10.3799/dqkx.2020.335
    Jiang Xiaojun, Peng Yunbiao, Dong Xiaojie, Li Huaming, Tu Ying, 2021. The Remote Role of Mongolia-Okhotsk Ocean: Evidences from the Origin of Rhyolite Porphyry in Yangpangou Area, the Southeast of Inner Mongolia. Earth Science, 46(9): 3057-3073. doi: 10.3799/dqkx.2020.335
    Citation: Jiang Xiaojun, Peng Yunbiao, Dong Xiaojie, Li Huaming, Tu Ying, 2021. The Remote Role of Mongolia-Okhotsk Ocean: Evidences from the Origin of Rhyolite Porphyry in Yangpangou Area, the Southeast of Inner Mongolia. Earth Science, 46(9): 3057-3073. doi: 10.3799/dqkx.2020.335

    蒙古-鄂霍次克洋的远程作用:来自内蒙古东南部羊盘沟地区流纹斑岩成因的证据

    doi: 10.3799/dqkx.2020.335
    基金项目: 

    中国核工业地质局铀矿勘查项目 2018-15

    中国核工业地质局铀矿勘查项目 202004-1

    详细信息
      作者简介:

      蒋孝君(1987-), 男, 工程师, 主要从事构造及铀矿勘查与研究, ORCID: 0000-0003-0105-1152.E-mail: 523990392@qq.com

    • 中图分类号: P581

    The Remote Role of Mongolia-Okhotsk Ocean: Evidences from the Origin of Rhyolite Porphyry in Yangpangou Area, the Southeast of Inner Mongolia

    • 摘要: 为了解蒙古—鄂霍次克构造体系的远程作用及其在中国东北以南的影响范围,在内蒙古多伦火山盆地羊盘沟地区开展了流纹斑岩锆石U-Pb同位素年代学、岩石地球化学及区域对比研究.结果显示,其形成时代为144.2±0.6 Ma,属于早白垩世早期.主量元素SiO2含量为73.25%~76.72%,K2O含量为4.64%~7.87%,K2O/Na2O值在1.15~3.82之间,A/CNK值为0.79~0.99;副矿物为磁铁矿、锆石和磷灰石等,属准铝质高钾钙碱性—钾玄岩系列A2型流纹岩类;稀土元素总量高(320.76×10-6~415.70×10-6),富集轻稀土元素、大离子亲石元素K和Rb、高场强元素Zr和Hf以及元素U、Th等,亏损重稀土元素、大离子亲石元素Ba和Sr、高场强元素Nb和Ta以及元素P、Ti等,显著Eu负异常(δEu=0.08~0.15).表明流纹斑岩形成于后碰撞构造环境,是早白垩世蒙古—鄂霍次克洋闭合后某个伸展事件下的产物,因此,蒙古—鄂霍次克构造体系在中国的影响范围向东南至少延伸至蒙东南—冀北一带,且对应的蒙古—鄂霍次克洋东段的闭合完成时间应早于144.2 Ma.

       

    • 图  1  羊盘沟地区构造位置图(a)及地质简图(b)

      图a据张长厚等(2006)许文良等(2013)修改. 1.第四系;2.白音高老组;3.满克头鄂博组;4.白音高老期流纹斑岩;5.白音高老期正长斑岩;6.流纹质熔结凝灰岩;7.流纹质含角砾凝灰岩;8.石英粗面质含角砾凝灰岩;9流纹岩;10.流纹斑岩;11.正长斑岩;12.地质界线;13.岩性界线;14.喷发不整合界线,15.区域断裂;16.正断层;17.钻孔位置

      Fig.  1.  Structural location (a) and geological sketch map (b) of Yangpangou area

      图  2  多伦火山盆地中生代以来地层格架

      Fig.  2.  Stratigraphic framework of Duolun volcanic basin since Mesozoic

      图  3  羊盘沟地区流纹斑岩宏观特征(a)和微观特征(b)

      Qtz.石英;Pl.斜长石;Kfs.钾长石

      Fig.  3.  Macro (a) and micro (b) characteristics of rhyolitic porphyry in Yangpangou area

      图  4  羊盘沟地区流纹斑岩部分锆石CL图像

      Fig.  4.  CL images of selected zircons for rhyolitic porphyry in Yangpangou area

      图  5  羊盘沟地区流纹斑岩锆石LA-ICP-MS U-Pb同位素年龄谐和图(a)和年龄分布直方图(b)

      Fig.  5.  U-Pb concordian diagram (a) and histogram (b) of zircons from rhyolitic porphyry in Yangpangou area

      图  6  羊盘沟地区流纹斑岩TAS图解(a)、K2O-SiO2图解(b)和A/NK-A/CNK图解(c)

      Fig.  6.  TAS diagram (a), K2O vs. SiO2 diagram (b) and A/NK vs. A/CNK diagram (c) of rhyolitic porphyry in Yangpangou area

      图  7  羊盘沟地区流纹斑岩稀土球粒陨石元素标准化分布型式图(a)和微量元素原始地幔标准化蛛网图(b)

      标准化值据Sun and McDonough(1989)

      Fig.  7.  Chondrite-normalized REE (a) and primitive mantle-normalized (b) diagrams of rhyolitic porphyry in Yangpangou area

      图  8  羊盘沟地区流纹斑岩(K2O+Na2O)/CaO-Zr+Nb+Ce+Y图解(a)、FeOT/MgO-Zr+Nb+Ce+Y图解(b)、(K2O+Na2O)/CaO-10 000Ga/Al图解(c)和Ce-10 000Ga/Al图解(d)

      A. A型;I & S. I、S型;FG. 分异的I、S型;OTG. 未分异的I、S型

      Fig.  8.  (K2O+Na2O)/CaO vs. Zr+Nb+Ce+Y (a)、FeOT/MgO vs. Zr+Nb+Ce+Y (b)、(K2O+Na2O)/CaO vs. 10 000Ga/Al (c) and Ce vs. 10 000Ga/Al (d) diagrams of rhyolitic porphyry in Yangpangou area

      图  9  羊盘沟地区流纹斑岩Nb-Y-Ce图解(a)和Nb-Y-3Ga图解(b)

      Fig.  9.  Nb-Y-Ce (a) and Nb-Y-3Ga (b) diagrams of rhyolitic porphyry in Yangpangou area

      图  10  羊盘沟地区流纹斑岩δEu-Sr源区判别图解

      Huo(1986)

      Fig.  10.  The δEu vs. Sr diagram of rhyolitic porphyry in Yangpangou area

      图  11  东北地区早白垩世早期和中晚侏罗世火山岩分布

      Huo(1986)

      Fig.  11.  Distribution map of early Early Cretaceous and Middle-Late Jurassic volcanic rocks in NE China

      图  12  羊盘沟地区流纹斑岩Rb-Y+Nb(a)和Nb-Y(a)构造环境判别图解

      Pearce(1983)

      Fig.  12.  Rb vs. Y+Nb (a) and Nb vs. Y (b) diagrams of rhyolitic porphyry in Yangpangou area

      图  13  早白垩世早期蒙东南‒冀北地区构造环境示意

      张超(2020)修改

      Fig.  13.  Schematic diagram of tectonic setting for the area between the southeast of Inner Mongolia and the north of Hebei during early Early Cretaceous

      表  1  羊盘沟地区流纹斑岩锆石LA⁃ICP⁃MS U⁃Pb同位素定年数据

      Table  1.   Zircon U⁃Pb dating of rhyolitic porphyry in Yangpangou area

      测点号 元素含量(10-6) Th/U 同位素比值 同位素年龄(Ma) 谐和度(%)
      Pb Th U 207Pb/206Pb 207Pb/235U 206Pb/238U 207Pb/206Pb 207Pb/235U 206Pb/238U
      测值 1σ 测值 1σ 测值 1σ 测值 1σ 测值 1σ 测值 1σ
      1 17 305 645 0.47 0.048 5 0.000 8 0.151 3 0.002 7 0.022 5 0.000 2 124.2 40.7 143.0 2.4 143.6 1.3 99
      2 19 363 676 0.54 0.049 2 0.000 9 0.153 1 0.002 8 0.022 6 0.000 2 166.8 38.0 144.7 2.4 143.9 1.3 99
      3 75 1 590 431 3.69 0.066 6 0.001 1 0.224 7 0.007 0 0.024 2 0.000 3 833.3 33.3 205.8 5.8 154.4 1.7 71
      4 27 433 1 021 0.42 0.050 4 0.000 7 0.157 0 0.002 3 0.022 5 0.000 2 213.0 33.3 148.0 2.0 143.6 1.1 96
      5 67 1 242 521 2.39 0.049 7 0.000 6 0.164 7 0.003 0 0.023 9 0.000 2 183.4 21.3 154.8 2.7 152.4 1.4 98
      6 30 502 1 124 0.45 0.050 4 0.000 7 0.157 3 0.002 4 0.022 6 0.000 2 213.0 33.3 148.4 2.1 143.8 1.2 96
      7 38 849 1 402 0.61 0.067 0 0.001 4 0.196 7 0.004 1 0.021 2 0.000 2 838.9 42.6 182.3 3.5 135.1 1.0 70
      8 21 376 766 0.49 0.049 4 0.000 9 0.154 5 0.002 8 0.022 7 0.000 2 164.9 40.7 145.9 2.5 144.4 1.3 98
      9 38 882 1 302 0.68 0.049 6 0.000 8 0.160 7 0.002 5 0.023 4 0.000 2 176.0 35.2 151.4 2.2 149.4 1.3 98
      10 42 695 1 568 0.44 0.049 7 0.000 8 0.155 6 0.002 5 0.022 6 0.000 2 189.0 37.0 146.9 2.2 144.2 1.2 98
      11 27 543 972 0.56 0.048 8 0.000 8 0.151 9 0.002 6 0.022 5 0.000 2 200.1 40.7 143.6 2.3 143.6 1.3 99
      12 20 351 740 0.47 0.049 1 0.000 9 0.152 2 0.002 7 0.022 5 0.000 2 150.1 44.4 143.9 2.4 143.4 1.2 99
      13 10 207 384 0.54 0.050 6 0.001 1 0.156 9 0.003 4 0.022 5 0.000 2 233.4 50.0 148.0 3.0 143.2 1.4 96
      14 39 631 1 443 0.44 0.049 9 0.000 8 0.156 4 0.002 4 0.022 6 0.000 2 190.8 37.0 147.5 2.1 144.2 1.2 97
      15 12 254 432 0.59 0.049 6 0.001 1 0.154 9 0.003 6 0.022 6 0.000 2 189.0 53.7 146.2 3.1 144.1 1.3 98
      16 11 223 406 0.55 0.047 8 0.001 0 0.153 0 0.003 1 0.023 2 0.000 2 100.1 78.7 144.6 2.7 147.7 1.3 97
      17 32 717 1 192 0.60 0.050 0 0.000 8 0.154 9 0.002 4 0.022 4 0.000 2 194.5 32.4 146.3 2.1 142.9 1.2 97
      18 17 316 619 0.51 0.048 4 0.000 8 0.150 0 0.002 5 0.022 5 0.000 2 116.8 45.4 141.9 2.2 143.4 1.3 98
      19 8 193 266 0.73 0.049 4 0.001 3 0.151 9 0.003 8 0.022 5 0.000 2 164.9 65.7 143.6 3.4 143.5 1.6 99
      20 17 385 573 0.67 0.066 3 0.001 5 0.207 7 0.005 1 0.022 5 0.000 2 814.5 48.9 191.6 4.3 143.7 1.3 71
      21 24 512 894 0.57 0.050 2 0.000 8 0.156 1 0.002 5 0.022 5 0.000 2 205.6 38.9 147.3 2.2 143.5 1.2 97
      22 8 215 293 0.73 0.048 4 0.001 2 0.150 0 0.003 9 0.022 5 0.000 3 116.8 59.3 141.9 3.4 143.4 1.8 98
      23 15 353 542 0.65 0.049 8 0.001 0 0.155 9 0.003 2 0.022 7 0.000 2 183.4 13.9 147.1 2.8 144.6 1.5 98
      24 20 342 764 0.45 0.049 5 0.000 8 0.154 0 0.002 6 0.022 5 0.000 2 172.3 38.9 145.4 2.3 143.6 1.3 98
      25 18 369 672 0.55 0.048 2 0.000 9 0.149 9 0.002 6 0.022 6 0.000 2 109.4 42.6 141.8 2.3 143.9 1.2 98
      26 7 203 248 0.82 0.050 2 0.001 4 0.155 6 0.004 5 0.022 5 0.000 3 205.6 97.2 146.8 4.0 143.3 1.6 97
      27 16 333 577 0.58 0.048 1 0.001 0 0.150 5 0.003 1 0.022 7 0.000 2 105.6 50.0 142.4 2.8 144.6 1.3 98
      28 58 1 353 1 173 1.15 0.049 4 0.000 6 0.158 8 0.002 2 0.023 2 0.000 2 168.6 25.9 149.6 2.0 148.1 1.0 98
      29 9 153 331 0.46 0.049 4 0.001 2 0.154 5 0.003 8 0.022 7 0.000 2 168.6 62.0 145.8 3.3 144.8 1.4 99
      30 14 285 524 0.54 0.048 5 0.000 9 0.151 0 0.002 8 0.022 5 0.000 2 124.2 40.7 142.8 2.5 143.5 1.2 99
      下载: 导出CSV

      表  2  羊盘沟地区流纹斑岩地球化学分析结果

      Table  2.   Geochemical dating of rhyolitic porphyry in Yangpangou area

      样品号 YP-1 YP-2 YP-3 YP-4 YP-5 H-ZKYP7-1 H-ZKYP7-2 H-ZKYP7-3
      SiO2 73.25 73.25 74.06 74.70 76.72 73.75 74.86 74.24
      TiO2 0.22 0.20 0.20 0.19 0.14 0.21 0.23 0.21
      Al2O3 12.65 12.50 12.33 12.05 11.41 12.50 12.22 12.36
      FeOT 2.73 2.69 1.61 1.62 1.63 2.15 2.15 2.01
      MnO 0.36 0.34 0.28 0.27 0.21 0.06 0.07 0.09
      MgO 0.09 0.08 0.21 0.19 0.16 0.24 0.19 0.11
      CaO 0.54 0.71 1.65 1.68 1.12 0.98 0.72 2.26
      Na2O 2.08 2.06 2.42 3.18 2.98 2.20 2.80 4.05
      K2O 7.87 7.87 6.82 5.69 5.43 7.87 6.73 4.64
      P2O5 0.03 0.03 0.03 0.02 0.01 0.04 0.04 0.03
      LOI 1.05 0.98 1.90 1.86 1.43 1.30 0.96 2.34
      DI 92.64 92.35 90.42 90.83 93.07 93.08 93.68 90.26
      A/CNK 0.99 0.95 0.86 0.84 0.89 0.90 0.93 0.79
      A/NK 1.07 1.06 1.09 1.06 1.06 1.04 1.04 1.06
      La 94.8 91.0 88.3 89.6 70.7 96.8 83.7 88.6
      Ce 180 177 168 172 141 182 158 166
      Pr 19.15 18.85 17.40 17.90 15.10 19.90 17.40 18.00
      Nd 66.3 65.1 59.9 61.8 52.2 71.7 63.4 66.2
      Sm 12.05 11.60 10.75 11.50 10.30 12.50 11.10 11.20
      Eu 0.530 0.430 0.400 0.430 0.250 0.409 0.388 0.334
      Gd 9.33 9.39 8.61 8.61 8.47 11.10 9.69 9.80
      Tb 1.42 1.54 1.36 1.42 1.46 1.69 1.46 1.49
      Dy 8.01 8.59 7.55 7.62 8.25 8.26 6.93 7.38
      Ho 1.53 1.74 1.46 1.50 1.74 1.51 1.22 1.34
      Er 4.24 5.04 4.12 4.55 4.99 4.34 3.54 3.91
      Tm 0.70 0.74 0.67 0.67 0.76 0.58 0.47 0.54
      Yb 4.22 4.56 4.03 4.00 4.80 4.33 3.50 4.01
      Lu 0.68 0.72 0.62 0.61 0.74 0.58 0.48 0.55
      ΣREE 402.96 395.80 372.67 381.71 320.76 415.70 361.28 379.35
      (La/Yb)N 15.18 13.49 14.81 15.14 9.95 15.11 16.16 14.93
      δEu 0.15 0.12 0.12 0.13 0.08 0.10 0.11 0.10
      Rb 323 313 265 219 209 272 220 143
      Ba 270 274 241 164 142 215 217 162
      Th 31.0 33.2 31.8 30.5 32.8 30.7 28.2 30.6
      U 6.54 5.60 150.00 36.50 32.90 3.20 4.50 5.12
      Ta 2.30 2.40 2.20 2.10 2.30 2.28 2.23 2.18
      Nb 24.7 25.0 22.9 23.0 24.4 28.9 29.6 25.6
      Sr 23.9 23.8 27.6 23.7 19.7 22.4 21.2 42.0
      Zr 443 451 426 402 348 174 163 172
      Hf 12.10 12.50 11.40 11.10 10.40 7.46 7.03 7.61
      Y 44.3 48.8 40.8 42.4 47.5 43.4 36.1 38.6
      Ga 24.4 23.2 23.6 23.1 22.7 24.3 24.2 21.8
      Rb/Sr 13.51 13.15 9.60 9.24 10.61 12.14 10.38 3.40
      Ti/Y 30.14 24.94 28.73 27.48 17.93 28.69 38.23 32.60
      Ti/Zr 3.01 2.70 2.75 2.90 2.45 7.16 8.47 7.32
      注:主量元素单位为%;稀土和微量元素单位为10-6;主量元素数据经过烧失量校正.
      下载: 导出CSV
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    • 收稿日期:  2020-08-11
    • 网络出版日期:  2021-10-14
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