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    大兴安岭北段中—新生代玄武岩成分变异:对地幔热演化过程意义

    唐杰 许文良 李宇 孙晨阳

    唐杰, 许文良, 李宇, 孙晨阳, 2019. 大兴安岭北段中—新生代玄武岩成分变异:对地幔热演化过程意义. 地球科学, 44(4): 1096-1112. doi: 10.3799/dqkx.2019.055
    引用本文: 唐杰, 许文良, 李宇, 孙晨阳, 2019. 大兴安岭北段中—新生代玄武岩成分变异:对地幔热演化过程意义. 地球科学, 44(4): 1096-1112. doi: 10.3799/dqkx.2019.055
    Tang Jie, Xu Wenliang, Li Yu, Sun Chenyang, 2019. Composition Variations of Mesozoic and Cenozoic Basalts in Northern Great Xing'an Range: Implications for Thermal Evolution of Mantle. Earth Science, 44(4): 1096-1112. doi: 10.3799/dqkx.2019.055
    Citation: Tang Jie, Xu Wenliang, Li Yu, Sun Chenyang, 2019. Composition Variations of Mesozoic and Cenozoic Basalts in Northern Great Xing'an Range: Implications for Thermal Evolution of Mantle. Earth Science, 44(4): 1096-1112. doi: 10.3799/dqkx.2019.055

    大兴安岭北段中—新生代玄武岩成分变异:对地幔热演化过程意义

    doi: 10.3799/dqkx.2019.055
    基金项目: 

    国家自然科学基金项目 41772047

    国家自然科学基金项目 91858211

    国家自然科学基金项目 41702051

    详细信息
      作者简介:

      唐杰(1989-), 女, 副教授, 博士, 主要从事火成岩岩石学研究

    • 中图分类号: P581

    Composition Variations of Mesozoic and Cenozoic Basalts in Northern Great Xing'an Range: Implications for Thermal Evolution of Mantle

    • 摘要: 近年来,东北地区地幔热演化过程的相关研究相对较少,而揭示东北地区地幔热演化过程的有效手段就是研究东北地区玄武岩的成分变异特征.系统总结并对比了大兴安岭北段早白垩世玄武质岩石和新生代玄武质岩石的化学成分变异,以便揭示研究区中生代晚期-新生代的地幔热演化过程.大兴安岭北段早白垩世玄武岩在化学上属于拉斑玄武岩系列,以亏损Nb、Ta、Ti等高场强元素为特征,它们的La/Nb和La/Ta比值分别介于1.8~5.6和30~87,暗示岩浆起源于岩石圈地幔;它们的初始87Sr/86Sr值、εNdt)和εHft)值分别介于0.704 5~0.706 9、-1.52~+3.60和+1.74~+7.77,表明岩浆源区属于弱亏损-弱富集的岩石圈地幔;早白垩世玄武质岩石的Sr-Nd-Pb同位素成分指示岩浆源区是由DM和EMⅡ型地幔端元混合而成,并经历了俯冲流体的交代.表明大兴安岭北段早白垩世玄武质岩浆源区为受早期俯冲流体交代的岩石圈地幔.新生代超钾质和钾质玄武岩具有Nb-Ta的弱负异常,87Sr/86Sr值为0.704 7~0.705 7、εNdt)值为-6.3~-0.8,而地幔捕掳体具有Sr-Nd同位素亏损特征;钠质玄武岩具有Nb-Ta的正异常,较超钾质和钾质玄武岩具有低的87Sr/86Sr(0.703 5~0.704 2)以及高的εNdt)值(+3.4~+6.6),类似MORB的同位素组成,这些特征说明大兴安岭北段新生代玄武质岩石起源于软流圈地幔.综上所述,大兴安岭北段早白垩世和新生代玄武质岩石成分的差异不仅指示其岩浆源区从岩石圈地幔转变为软流圈地幔,更为重要的是它揭示了研究区地幔的热演化过程——从早白垩世高的地温梯度到新生代低的地温梯度的转变.这一过程也是岩石圈从中生代晚期到新生代逐渐增厚的过程.结合区域构造演化,可以得出大兴安岭北段早白垩世的玄武质岩浆作用与岩石圈伸展、减薄形成的裂陷作用相关,而新生代玄武质岩浆作用则与陆内裂谷作用相关.

       

    • 图  1  大兴安岭北段中-新生代玄武质岩石分布

      Wu et al.(2011); Xu et al.(2013)

      Fig.  1.  Distribution of the Mesozoic-Cenozoic basalts in the northern Great Xing'an Range

      图  2  大兴安岭北段中生代玄武质岩石的TAS图解(a)和SiO2-K2O图解(b)

      图a据Le Bas et al.(1986); 图b据Peccerillo and Taylor, 1976; 数据来源:未发表数据;Fan et al.(2003)Zhang et al.(2008)葛文春等(1999, 2000);林强等(2003)孟恩等(2011)徐美君等(2011);阴影区代表大兴安岭北段新生代玄武质岩石,引自Zhang et al.(1995); Chen et al.(2007); Ho et al.(2013); Kuritani et al.(2013); Sun et al.(2014); Zhao et al.(2014); Li et al.(2018)

      Fig.  2.  Plots of TAS (a) and SiO2 versus K2O (b) for the Mesozoic basalts in the northern Great Xing'an Range

      图  3  大兴安岭北段中生代玄武质岩石的Sm/Nd-εHf(t)图解

      数据来源见图 2

      Fig.  3.  Plot of Sm/Nd-εHf(t) for the Mesozoic basalts in the northern Great Xing'an Range

      图  4  大兴安岭北段中生代玄武质岩石的Hark图解

      数据来源见图 2,不包括塔河玄武岩

      Fig.  4.  Hark diagrams for the Mesozoic basalts in the northern Great Xing'an Range

      图  5  大兴安岭北段中生代玄武质岩石的La-La/Sm图解

      数据来源见图 2,不包括塔河玄武岩

      Fig.  5.  Plot of La-La/Sm for the Mesozoic basalts in the northern Great Xing'an Range

      图  6  大兴安岭北段中-新生代玄武质岩石球粒陨石标准化稀土元素配分图(a); 原始地幔标准化微量元素蛛网图(b)

      图a中标准化数值据Boynton (1984); 图b中标准化数值据Sun and McDonough (1989); 中生代玄武质岩石数据来源见图 2;新生代玄武质岩石数据为平均值, 来源:Zhang et al.(1995); Chen et al.(2007); Ho et al.(2013); Kuritani et al.(2013); Sun et al.(2014); Zhao et al.(2014); Liu et al.(2017)

      Fig.  6.  Chondrite-normalized REE patterns (a) and primitive-mantle-normalized trace element spidergrams (b) for the Mesozoic-Cenozoic basalts in the northern Great Xing'an Range

      图  7  大兴安岭北段中-新生代玄武质岩石的εNd(t)-εHf(t)(a)和(87Sr/86Sr)i-εNd(t)(b)图解

      A.新生代超钾质-钾质玄武岩;B.新生代钠质玄武岩;BSE.全硅酸盐地球值;MORB.洋脊玄武岩;OIB.大洋岛屿玄武岩;IAB.岛弧玄武岩;全球阵列参考线εHf(t)=1.36εNd(t)+2.95,引自Vervoort and Blichert-Toft (1999);Basin and Range.美国盆岭地区新生代火山岩,引自Hawkesworth et al.(1995)Rogers et al.(1995);PM.原始地幔;EMI.I型富集地幔,EMII.II型富集地幔,引自Zindle and Hart (1986)

      Fig.  7.  Plots of εNd(t)-εHf(t) (a) and (87Sr/86Sr)i-εNd(t)(b) for the Mesozoic-Cenozoic basalts in the northern Great Xing'an Range

      图  8  大兴安岭北段中-新生代玄武质岩石全岩Sr-Nd-Pb同位素协变图

      图例见图 7;A.新生代超钾质-钾质玄武岩;B.新生代钠质玄武岩;HIMU.高238U/204Pb值地幔;EMI、EMII、MORB数据来自GEOROC

      Fig.  8.  Variations of Sr-Nd-Pb isotopic compositions for the Mesozoic-Cenozoic basalts in the northern Great Xing'an Range

      图  9  大兴安岭北段中生代玄武质岩石的SiO2-Zr/Y(a)和SiO2-Sr图解(b)

      图例见图 7;美国盆岭地区新生代火山岩和日本岛弧火山岩引自Hawkesworth et al.(1995)Rogers et al.(1995)

      Fig.  9.  Plots of SiO2-Zr/Y (a) and SiO2-Sr (b) for the Mesozoic basalts in the northern Great Xing'an Range

      图  10  大兴安岭北段中-新生代玄武质岩石形成过程

      a.中生代晚期玄武质岩浆起源深度约为46 km,源区为受早期俯冲流体交代的岩石圈地幔;b.新生代玄武质岩浆起源深度约为120~150 km,源区为具有EMI特征的再循环地壳物质

      Fig.  10.  Simplified carton describing formation process of the Mesozoic-Cenozoic basalts in the northern Great Xing'an Range

      表  1  大兴安岭北段早白垩世玄武质岩石定年结果

      Table  1.   Geochronological data for the Early Cretaceous basalts in the northern Great Xing'an Range

      样品号 采样位置 岩性 年龄(Ma) 测年方法 文献
      12ER21 50°09′40″N 120°11′58″E 玄武安山岩 119±1 40Ar-39Ar 未发表数据
      ER1 49°59′57″N 120°06′50″E 粗安岩 128±2 LA-ICPMS 徐美君等,2011
      ER3 50°19′57″N 120°15′01″E 玄武粗安岩 125±3 LA-ICPMS 徐美君等,2011
      ER5-1 50°26′01″N 120°00′54″E 安山岩 114±3 LA-ICPMS 徐美君等,2011
      ER19-1 50°42′37″N 120°12′52″E 玄武安山岩 127±1 LA-ICPMS 徐美君等,2011
      MZ10-1 49°23′56″N 117°25′21″E 辉石安山岩 125±2 LA-ICPMS 孟恩等,2011
      MZ21-1 49°26′42″N 117°02′31″E 橄榄玄武岩 129±2 LA-ICPMS 孟恩等,2011
      14ER19-1 51°43′05″N 120°44′43″E 玄武安山岩 132±2 SIMS Zhao et al., 2016
      14ER20-1 51°43′05″N 120°44′43″E 玄武安山岩 126±2 SIMS Zhao et al., 2016
      FW04-420 48°16′31″N 123°38′12″E 玄武安山岩 123±2 LA-ICPMS Zhang et al., 2008
      GW04257 48°09′13″N 121°14′44″E 玄武岩 128±8 LA-ICPMS Zhang et al., 2008
      GW04027 48°51′11″N 121°37′27″E 玄武岩 112±2 40Ar-39Ar Zhang et al., 2008
      GW04032 49°07′01″N 120°55′43″E 玄武岩 118±1 40Ar-39Ar Zhang et al., 2008
      ELC04-1 50°40′04″N 122°35′57″E 玄武岩 125±1 40Ar-39Ar Wang et al., 2006
      TH08 52°19′30″N 124°40′40″E 玄武岩 124±1 40Ar-39Ar Wang et al., 2006
      TH24 52°39′38″N 124°19′38″E 玄武安山岩 126±1 40Ar-39Ar Wang et al., 2006
      TH22 52°39′39″N 124°19′42″E 玄武岩 122±1 40Ar-39Ar Wang et al., 2006
      GH07 50°19′54″N 120°14′53″E 玄武岩 123±1 40Ar-39Ar Wang et al., 2006
      GH10 50°26′23″N 120°48′13″E 玄武岩 121±1 40Ar-39Ar Wang et al., 2006
      YKSNQ04-4 49°12′22″N 120°36′50″E 玄武岩 116±1 40Ar-39Ar Wang et al., 2006
      YKSNQ04-1 49°12′47″N 120°36′50″E 玄武安山岩 114±1 40Ar-39Ar Wang et al., 2006
      ZLT04-8 48°00′18″N 122°48′23″E 玄武安山岩 122±1 40Ar-39Ar Wang et al., 2006
      YKS04-3 48°50′47″N 121°34′58″E 玄武粗安岩 106±1 40Ar-39Ar Wang et al., 2006
      GH04-1 50°21′32″N 120°26′49″E 粗玄岩 124±1 40Ar-39Ar Wang et al., 2006
      GH04-4 50°59′17″N 121°19′16″E 玄武粗安岩 115±1 40Ar-39Ar Wang et al., 2006
      JGD04-4 49°56′53″N 124°22′48″E 玄武岩 115±1 40Ar-39Ar Wang et al., 2006
      下载: 导出CSV
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