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饶河杂岩中枕状玄武岩的锆石U－Pb年代学、地球化学及其地质意义

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曾振, 孙雷, 张兴洲, 崔维龙, 蒋力. 饶河杂岩中枕状玄武岩的锆石U－Pb年代学、地球化学及其地质意义[J]. 地质与资源, 2019, 28(2): 119-127.
引用本文: 曾振, 孙雷, 张兴洲, 崔维龙, 蒋力. 饶河杂岩中枕状玄武岩的锆石U－Pb年代学、地球化学及其地质意义[J]. 地质与资源, 2019, 28(2): 119-127.
shu
ZENG Zhen, SUN Lei, ZHANG Xing-zhou, CUI Wei-long, JIANG Li. ZIRCON U-Pb CHRONOLOGY AND GEOCHEMISTRY OF THE PILLOW BASALTS FROM RAOHE COMPLEX: Geological Implications[J]. Geology and Resources, 2019, 28(2): 119-127.
Citation: ZENG Zhen, SUN Lei, ZHANG Xing-zhou, CUI Wei-long, JIANG Li. ZIRCON U-Pb CHRONOLOGY AND GEOCHEMISTRY OF THE PILLOW BASALTS FROM RAOHE COMPLEX: Geological Implications[J]. Geology and Resources, 2019, 28(2): 119-127.
shu

饶河杂岩中枕状玄武岩的锆石U－Pb年代学、地球化学及其地质意义

  • 1.

    航天建筑设计研究院有限公司, 北京 100162

  • 2.

    吉林大学 地球科学学院, 吉林 长春 130061

  • 3.

    中国地质调查局 沈阳地质调查中心, 辽宁 沈阳 110034

  • 基金项目:
    国家自然科学基金重点项目“兴蒙海槽晚古生代构造演化”（编号40739905）；中国地质调查局项目“黑龙江省东部隐伏盆地页岩气地质条件综合调查”（编号1212011120973）；“松辽外围西部盆地油气基础地质调查”（编号DD20160163）
详细信息
    作者简介: 曾振(1989-), 男, 博士, 工程师, 主要从事区域大地构造及工程地质方向研究, 通信地址北京市大兴区西红门镇春和路39号院, E-mail//23911989@qq.com
    通讯作者: 孙雷(1988-), 男, 硕士, 工程师, 主要从事油气基础地质调查研究工作, 通信地址辽宁省沈阳市皇姑区黄河北大街280号, E-mail//sunlei2326@126.com

  • 中图分类号: P588.14;P597;P595

ZIRCON U-Pb CHRONOLOGY AND GEOCHEMISTRY OF THE PILLOW BASALTS FROM RAOHE COMPLEX: Geological Implications

  • 1.

    China Aerospace Architectural Design and Research Institute Co., Ltd., Beijing 100162, China

  • 2.

    College of Earth Sciences, Jilin University, Changchun 130061, China

  • 3.

    Shenyang Center of Geological Survey, CGS, Shenyang 110034, China

More Information

    摘要

  • 那丹哈达增生杂岩为中国东部古太平洋板块俯冲最为可靠的地质记录之一，对限定古大洋板块的西向俯冲具有重要的理论意义.饶河杂岩位于那丹哈达增生杂岩的核心位置，发育典型的增生杂岩组合，其中玄武岩类多呈构造透镜体状产出于超镁铁质-镁铁质杂岩带，变形轻微，没有遭受变质.对饶河杂岩中枕状玄武岩样品进行的同位素年代学和地球化学研究结果表明：饶河杂岩中枕状玄武岩锆石LA-ICP-MS U-Pb年龄为中侏罗世（168±2 Ma），枕状玄武岩大离子亲石元素Rb、Sr亏损，高场强元素Nb、Ta富集，Th元素丰度较高，形成于洋岛（OIB型）环境.饶河杂岩中枕状玄武岩的形成时代和成因环境，对于该区侏罗纪时期构造动力学背景研究具有意义.

    As one of the most reliable geological records of paleo-Pacific Plate subduction in eastern China, the Nadanhada accretionary complex is of great importance to define the westward subduction of paleo-oceanic plate. The Raohe Complex is located in the core of the complex, developed with typical accretionary complex association, among which the basaltoids, mostly in structural lenticles, are occurred in the ultramafic-mafic complex zone with slight deformation but no metamorphism. Study on the isotopic chronology and geochemistry of the pillow basalt samples from Raohe Complex shows that the LA-ICP-MS zircon U-Pb age is Middle Jurassic(168±2 Ma), with depletion of LILEs (Rb and Sr), enrichment of HFSEs(Nb and Ta) and high-abundant Th, which was formed in the ocean island environment (OIB). Its formation age and genetic environment is significant to study the tectonic dynamic background of the area during the Jurassic period.

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  • 图 1  中国东北及其邻区大地构造及那丹哈达地体地质简图（据文献[2]）

    Figure 1. 

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    图 2  饶河杂岩中的枕状玄武岩野外露头照片

    Figure 2. 

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    图 3  饶河杂岩中枕状玄武岩锆石阴极发光图像及U-Pb年龄谐和图

    Figure 3. 

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    图 4  饶河杂岩中枕状玄武岩岩石分类图解（据文献[33-34]）

    Figure 4. 

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    图 5  枕状玄武岩球粒陨石标准化稀土元素配分模式和原始地幔标准化微量元素蛛网图(球粒陨石和原始地幔标准化值据[37], 韵陨月值据[37-38])

    Figure 5. 

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    图 6  枕状玄武岩Ti/100-Zr-3Y和2Nb-Zr/4-Y构造判别图解(据文献[41])

    Figure 6. 

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    图 7  枕状玄武岩Zr/Yb-Zr和Nb/Yb-Th/Yb构造判别图解(据文献[42])

    Figure 7. 

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    表 1  饶河杂岩中枕状玄武岩样品(15HLJ28)的锆石LA-ICP-MS U-Pb测年结果

    Table 1.  LA-ICP-MS zircon U-Pb dating results of the pillow basalt sample 15HLJ28 from Raohe Complex

    元素含量/10-6 Th/U 同位素比值 年龄Ma
    Pb Th U 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ Conc
    58.3 431 639 0.67 0.0488 0.0035 0.1740 0.0127 0.0261 0.0004 200 94 163 11 166 3 97%
    352 3108 2382 1.31 0.0512 0.0020 0.1820 0.0068 0.0260 0.0003 250 86 170 6 165 2 97%
    45.9 342 482 0.71 0.0480 0.0044 0.1753 0.0161 0.0265 0.0005 98 204 164 14 169 3 97%
    74 584 723 0.81 0.0538 0.0035 0.1909 0.0119 0.0266 0.0006 365 146 177 10 169 4 95%
    55.3 396 609 0.65 0.0517 0.0037 0.1880 0.0133 0.0268 0.0007 276 165 175 11 170 4 97%
    98 782 1130 0.69 0.0496 0.0028 0.1775 0.0096 0.0268 0.0007 176 131 166 8 170 4 97%
    57.5 457 581 0.79 0.0539 0.0042 0.1924 0.0142 0.0267 0.0008 369 171 179 12 170 5 94%
    15.4 130 299 0.44 0.0530 0.0071 0.1805 0.0227 0.0268 0.0007 328 281 169 20 170 5 98%
    88 673 796 0.85 0.0527 0.0035 0.1896 0.0120 0.0265 0.0005 317 150 176 10 169 3 95%
    183 1550 1231 1.26 0.0482 0.0023 0.1795 0.0085 0.0274 0.0005 109 111 168 7 174 3 96%
    347 2936 1915 1.53 0.0470 0.0019 0.1755 0.0071 0.0272 0.0003 56 87 164 6 173 2 94%
    90 778 793 0.98 0.0497 0.0029 0.1794 0.0105 0.0261 0.0004 189 144 168 9 166 2 99%
    300 2492 1736 1.44 0.0482 0.0023 0.1787 0.0087 0.0267 0.0003 109 107 167 8 170 2 98%
    19.3 139 223 0.63 0.0497 0.0037 0.1822 0.0135 0.0264 0.0008 189 154 170 12 168 5 99%
    12.7 92.3 165 0.56 0.0490 0.0043 0.1767 0.0152 0.0264 0.0008 150 193 165 13 168 5 98%
    71 563 552 1.02 0.0475 0.0025 0.1756 0.0090 0.0269 0.0007 72 122 164 8 171 5 95%
    16.6 127 203 0.63 0.0502 0.0039 0.1811 0.0141 0.0262 0.0008 211 183 169 12 167 5 98%
    44.4 349 369 0.94 0.0527 0.0030 0.1897 0.0106 0.0264 0.0007 317 128 176 9 168 5 95%
    156 1367 775 1.76 0.0508 0.0023 0.1825 0.0080 0.0261 0.0007 232 102 170 7 166 4 97%
    81 674 554 1.22 0.0492 0.0023 0.1759 0.0084 0.0260 0.0007 167 111 165 7 165 4 99%
    15.9 117 172 0.68 0.0455 0.0043 0.1618 0.0147 0.0264 0.0008 — — 152 13 168 5 90%
    9.3 58.8 116 0.51 0.0615 0.0068 0.2041 0.0207 0.0255 0.0008 657 205 189 17 162 5 84%
    22.2 178 250 0.71 0.0461 0.0038 0.1607 0.0130 0.0254 0.0007 6 185 151 11 162 5 93%
    下载: 导出CSV

    表 2  饶河杂岩中枕状玄武岩地球化学分析结果

    Table 2.  Geochemical data of the pillow basalt in Raohe Complex

    样品 15HLJ28a 15HLJ28b 15HLJ28c 15HLJ28d
    SiO2 48.03 44.36 45.19 49.82
    TiO2 2.49 3.34 3.09 2.7
    Al2O3 11.52 12.1 12.62 13.9
    TFe2O3 14.8 13.62 12.51 10.52
    MnO 0.24 0.16 0.15 0.21
    MgO 7.67 9.19 9.63 6.17
    CaO 9.07 9.46 9.08 8.86
    Na2O 2.98 2.99 3.08 4.31
    K2O 0.6 0.29 0.26 0.32
    P2O5 0.73 0.8 0.73 0.61
    LOI 1.57 2.87 3.08 1.5
    Total 99.7 99.18 99.42 98.92
    Ba 261 93.9 63.2 236
    Rb 16.4 6.2 6.7 7.3
    Sr 337 289 236 553
    Zr 317 353 309 246
    Nb 69.8 73.4 67.5 59.6
    Ni 150 198 146.5 69.3
    Co 27.6 49.9 42.9 28.4
    Cr 260 310 270 30
    La 52.5 59 52.6 46.1
    Ce 109.1 114.5 107.5 87.7
    Pr 11.75 13.1 12.2 9.97
    Nd 48.3 53.9 50 39.6
    Sm 10.05 11.8 10.5 8.29
    Eu 3.3 3.93 3.46 2.94
    Gd 9.98 11.15 10.1 8.92
    Tb 1.25 1.41 1.38 1.17
    Dy 6.55 7.71 7.32 6.69
    Ho 1.19 1.29 1.24 1.11
    Er 2.71 2.87 2.93 2.73
    Tm 0.35 0.36 0.36 0.38
    Yb 1.81 1.83 1.91 1.96
    Lu 0.25 0.24 0.26 0.26
    Y 33.3 35.6 33.9 32.3
    Ta 4.4 4.7 4.4 3.6
    Hf 6.4 8 6.8 5.5
    V 178 237 250 226
    U 0.92 1.8 1.66 1.46
    Th 6.21 5.75 5.56 5.23
    Sc 13.6 22.1 22.0 17.2
    ∑REE 256.94 330.66 339.72 305.59
    LREE/HREE 9.76 9.54 9.27 8.38
    (La/Yb)N 19.56 21.74 18.57 15.86
    (Gd/Yb)N 4.45 4.92 4.27 3.67
    Eu/Eu* 1.00 1.03 1.49 1.54
    含量单位:主量元素为%, 稀土和微量元素为10-6(质量分数).
    下载: 导出CSV
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收稿日期:  2018-05-30
修回日期:  2018-11-15
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