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    额尔古纳地块早-中三叠世安山岩的发现及其对蒙古-鄂霍茨克洋南向俯冲的指示

    李强 程学芹 陈伟 刘洪章 张涛 张建珍 贾立民 杨宁 刘腾飞

    李强, 程学芹, 陈伟, 刘洪章, 张涛, 张建珍, 贾立民, 杨宁, 刘腾飞, 2021. 额尔古纳地块早-中三叠世安山岩的发现及其对蒙古-鄂霍茨克洋南向俯冲的指示. 地球科学, 46(8): 2768-2785. doi: 10.3799/dqkx.2020.319
    引用本文: 李强, 程学芹, 陈伟, 刘洪章, 张涛, 张建珍, 贾立民, 杨宁, 刘腾飞, 2021. 额尔古纳地块早-中三叠世安山岩的发现及其对蒙古-鄂霍茨克洋南向俯冲的指示. 地球科学, 46(8): 2768-2785. doi: 10.3799/dqkx.2020.319
    Li Qiang, Cheng Xueqin, Chen Wei, Liu Hongzhang, Zhang Tao, Zhang Jianzhen, Jia Limin, Yang Ning, Liu Tengfei, 2021. Discovery of Early-Middle Triassic Andesite in Erguna Massif and Its Indication of Southward Subduction of Mongol-Okhotsk Ocean Plate. Earth Science, 46(8): 2768-2785. doi: 10.3799/dqkx.2020.319
    Citation: Li Qiang, Cheng Xueqin, Chen Wei, Liu Hongzhang, Zhang Tao, Zhang Jianzhen, Jia Limin, Yang Ning, Liu Tengfei, 2021. Discovery of Early-Middle Triassic Andesite in Erguna Massif and Its Indication of Southward Subduction of Mongol-Okhotsk Ocean Plate. Earth Science, 46(8): 2768-2785. doi: 10.3799/dqkx.2020.319

    额尔古纳地块早-中三叠世安山岩的发现及其对蒙古-鄂霍茨克洋南向俯冲的指示

    doi: 10.3799/dqkx.2020.319
    基金项目: 

    中国地质调查局地质矿产调查项目 12120115032001

    国家自然科学基金项目 41902099

    详细信息
      作者简介:

      李强(1986-), 男, 硕士, 工程师, 主要从事岩石学与区域矿产地质调查研究.ORCID: 0000-0002-3239-8338.E-mail: 1032564223@qq.com

      通讯作者:

      陈伟, E-mail: nmgchenwei@163.com

    • 中图分类号: P581

    Discovery of Early-Middle Triassic Andesite in Erguna Massif and Its Indication of Southward Subduction of Mongol-Okhotsk Ocean Plate

    • 摘要: 安山岩与俯冲构造环境密切相关,对安山岩的研究可以获得俯冲作用发生时代及相关俯冲过程的重要信息.报道了大兴安岭北段、额尔古纳地块之上凤水山地区早-中三叠世安山岩的岩石学特征、锆石U-Pb年龄以及全岩地球化学数据,以揭示该地区蒙古-鄂霍茨克大洋板片南向俯冲作用的初始过程.凤水山地区安山岩的锆石多数呈自形-半自形短柱状、粒状,具有典型的震荡生长环带和高Th/U(0.23~1.34)比值,暗示其为岩浆成因锆石.锆石LA-MC-ICP-MS U-Pb同位素测年结果显示其分别形成于251±2 Ma和243±2 Ma,分属早三叠世和中三叠世,表明凤水山地区存在早中生代安山岩.这些早中生代安山岩的SiO2含量介于53.52%~60.38%,Al2O3含量介于16.17%~17.41%,Fe2O3T含量为5.55%~8.93%,MgO含量介于1.96%~5.97%,TiO2含量介于0.97%~1.67%,全碱(K2O+Na2O)含量为5.60%~8.05%,Na2O/K2O比值为1.23~2.51,铝饱和指数A/CNK介于0.86~0.97,具有较高的Mg#值(47~75),为钙碱性系列岩石.岩石样品富集Rb、Ba、U、K、Pb等大离子亲石元素和轻稀土元素,明显亏损Nb、Ta、Ti、P等高场强元素和重稀土元素,具有微弱的负Eu异常(δEu=0.74~0.99),与俯冲带大陆边缘弧岩浆岩地球化学特征类似.凤水山地区早中生代安山岩岩浆可能起源于幔源玄武质岩浆与壳源硅质熔体的混合作用,而幔源玄武质岩浆起源于俯冲板片沉积物或沉积物熔体改造的富集地幔,可能与前人提出的MASH(melting,assimilation,storage and homogenization)过程一致.因此,研究区三叠纪安山岩形成于蒙古-鄂霍茨克大洋板片南向俯冲相关的安第斯型活动大陆边缘环境.

       

    • 图  1  研究区地质图

      图a据纪政等(2018)修改. 1.中元古界兴华渡口岩群;2.新元古界-下寒武统倭勒根岩群;3.寒武纪花岗岩;4.晚二叠世-三叠纪闪长岩-花岗岩;5.早-中三叠世火山岩;6.早侏罗世石英二长闪长岩、斑状黑云母二长花岗岩;7.早白垩世中酸性火山岩;8早白垩世石英正长岩、正长斑岩;9.第四系;10.不整合界线/断层;11.取样位置及年龄

      Fig.  1.  Geological sketch map of the study area

      图  2  凤水山地区早-中三叠世安山岩及其显微照片

      a、b. 安山岩野外露头;c. 斜长石斑晶具环带结构;d. 安山岩中微晶闪长岩质包体;e. 辉石具联斑结构;f. 石英“眼斑”及辉石反应边. Q. 石英;Pl. 斜长石;Px. 辉石. 显微照片均在正交偏光下拍摄

      Fig.  2.  Field andesite and its microscopic photomicrographs in the Fengshui Mountain area

      图  3  凤水山地区安山岩锆石阴极发光(CL)图像与206Pb/238U年龄(a、b)及其U-Pb年龄谐和图(c、d)

      Fig.  3.  Cathodoluminescence(CL)images and 206Pb/238U ages (a, b) and concordia diagrams (c, d) for zircons from andesites in the Fengshui Mountain area

      图  4  凤水山地区安山岩TAS (a)和K2O-SiO2(b)图解

      底图据le Maitre(2002);南美安第斯陆弧中带火山岩数据引自Winter(2001)

      Fig.  4.  TAS diagram (a) and K2O-SiO2 diagram (b) for andesites in the Fengshui Mountain area

      图  5  凤水山地区安山岩球粒陨石标准化配分曲线(a)和微量元素原始地幔标准化蛛网图(b)

      球粒陨石和原始地幔标准值引自Sun and McDonough(1989);阴影部分数据及平均安第斯陆弧数据引自Winter(2001);平均俯冲沉积物数据引自Plank and Langmuir(1998);平均地壳数据引自Rudnick and Gao(2003)

      Fig.  5.  Chondrite-normalized REE pattern (a) and primitive mantle-normalized spider diagram (b) for andesites in the Fengshui Mountain area

      图  6  凤水山地区安山岩Sr/Y-Y(a)和Th/Yb-Ba/La(b)图解

      a. 底图据Defant and Drummond(1990);b. 底图据Woodhead et al.(2001)

      Fig.  6.  Diagrams of Sr/Y-Y (a) and Th/Yb-Ba/La (b) for andesites in the Fengshui Mountain area

      图  7  凤水山地区安山岩Th/Yb-Ta/Yb (a)和La/Yb-Sc/Ni (b) 图解

      a. 底图据Pearce(1982);b. 底图据Bailey(1981)

      Fig.  7.  Diagrams of Th/Yb-Ta/Yb (a) and La/Yb-Sc/Ni (b) for andesites in the Fengshui Mountain area

      图  8  凤水山地区安山岩Rb-SiO2 (a)和Rb-Sr(b)图解

      a. 底图据Ninkovich and Donn(1976);b. 底图据Condie(1973).图中数据为地壳厚度

      Fig.  8.  Diagrams of Rb-SiO2 (a) and Rb-Sr (b) for andesites in the Fengshui Mountain area

      表  1  凤水山地区安山岩微量元素特征与不同构造环境安山岩对比(参考数据来源于Condie,1989

      Table  1.   Trace element characteristics of andesites in the Fengshui Mountain area and comparison to andesites from various tectonic setting (reference values from Condie, 1989)

      参数 PAA
      (原始弧安山岩)
      IAA
      (岛弧安山岩)
      CMA
      (大陆边缘弧安山岩)
      AA
      (安第斯安山岩)
      研究区安山岩
      Th(10-6 ≤1 1~3 2~5 4~8 7.4~8.9
      La(10-6 2~5 5~15 10~25 20~40 39~61
      La/Yb ≤0.8 0.5~3.0 1~4 3~7 17~30
      Zr/Y ≤3 3~7 4~12 12~50 10~15
      Ti/V ≤30 20~40 20~50 20~70 50~66
      Hf/Yb ≤1 1~3 1~3 ≥3 3~5
      Ti/Zr > 50 40~50 40~50 ≤40 14~29
      下载: 导出CSV
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