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    华北克拉通燕山期岩浆活动的数值模拟

    乔彦超 刘翠 赵桂萍 石耀霖

    乔彦超, 刘翠, 赵桂萍, 石耀霖, 2012. 华北克拉通燕山期岩浆活动的数值模拟. 地球科学, 37(S1): 203-212. doi: 10.3799/dqkx.2012.S1.021
    引用本文: 乔彦超, 刘翠, 赵桂萍, 石耀霖, 2012. 华北克拉通燕山期岩浆活动的数值模拟. 地球科学, 37(S1): 203-212. doi: 10.3799/dqkx.2012.S1.021
    QIAO Yan-chao, LIU Cui, ZHAO Gui-ping, SHI Yao-lin, 2012. Numerical Simulation of the Magmatism of North China Craton during Yanshanian. Earth Science, 37(S1): 203-212. doi: 10.3799/dqkx.2012.S1.021
    Citation: QIAO Yan-chao, LIU Cui, ZHAO Gui-ping, SHI Yao-lin, 2012. Numerical Simulation of the Magmatism of North China Craton during Yanshanian. Earth Science, 37(S1): 203-212. doi: 10.3799/dqkx.2012.S1.021

    华北克拉通燕山期岩浆活动的数值模拟

    doi: 10.3799/dqkx.2012.S1.021
    基金项目: 

    国家自然科学基金项目 90814014

    ;国土资源部深部探测技术与实验研究专项 Sinoprobe-07

    中国科学院知识创新工程重要方向项目 kzcx2yw123

    详细信息
      作者简介:

      乔彦超(1985-),男,博士在读,固体地球物理,从事华北克拉通岩石圈破坏的数值模拟.E-mail: oliver.qiao@gmail.com

      通讯作者:

      石耀霖,shiyl@gucas.ac.cn

    • 中图分类号: P314.2

    Numerical Simulation of the Magmatism of North China Craton during Yanshanian

    • 摘要: 为了定量给出华北克拉通燕山期岩浆活动的规模,在合理构建华北燕山期地质-物理模型的基础上,利用有限元方法,在忽略玄武岩浆内对流只考虑热传导的假定下,反演了该区燕山期形成花岗岩所需要的侵入玄武岩浆的量.通过计算表明:(1)在压力1 GPa、地幔的玄武岩浆底侵作用于下地壳英云闪长岩围岩的情况下,英云闪长岩围岩的纯熔融量与底侵玄武岩纯结晶总量的比值约为0.161;假设仅有25%的熔浆可分离出来,则分离出的熔浆与玄武岩结晶总量比约为0.040 25.(2)数值模拟得到最后发生相变的整体区域为-50.285~-36.867 km.与前人研究得到的现今下地壳下部和壳幔过渡带33~40 m和40~50 km接近,表明此数值模拟方法具有可行性.

       

    • 图  1  1 GPa无水条件下4种岩石类型的熔体份额对温度的函数关系(Bergantz, 1989)

      a.玄武岩;b.英云闪长岩;c.白云母花岗岩;d.变泥质岩

      Fig.  1.  Melt fraction as a function of temperature for four rock types at 1 GPa

      图  2  玄武岩(a)和英云闪长岩(b)的数值化相变曲线

      Fig.  2.  Numerical phase transition curve of basalt (a) and tonalite (b)

      图  3  不同时刻温度场的分布情况

      图 3a3b、3c和3d分别为2.5、5.0、7.5和10.0 Ma后温度场分布情况,温度场彩色图标中,蓝色代表 0 ℃,红色代表 1 500 ℃;图中的2条温度等值线分别为850和1 250 ℃,即分别为围岩开始相变为熔融相和岩浆开始相变为固热混合相的温度

      Fig.  3.  Distribution of temperature at different times

      图  4  x=0剖面温度随时间变化曲线

      Fig.  4.  Temperature-time curve at x=0 section plane

      图  5  围岩和岩浆不同深度温度随时间的变化曲线

      Fig.  5.  Temperature-time curve at different depths for rock and magma

      图  6  围岩(a)和底侵玄武岩浆(b)在不同温度深度随时间的变化

      Fig.  6.  Depth-time curve at different temperatures for rock (a) and magma (b)

      表  1  围岩和岩浆热学参数

      Table  1.   Parameters of rock and magma

      L
      (kJ·kg-1)
      ρf
      (kg·m-3)
      ρw
      (kg·m-3)
      kf
      (W·m-1·K-1)
      kw
      (W·m-1·K-1)
      cf
      (J·kg-1/℃)
      cw
      (J·kg-1/℃)
      3.5×105 2.54 2.75 2.105 5 1.925 1 200 1 000
      注:ρfρw分别表示围岩和岩浆的密度;kfkw分别表示围岩和岩浆的导热系数;cfcw分别表示围岩和岩浆的容积热容量;数据参考崔承禹(1994)付明希等(2004)刘翠等(2006).
      下载: 导出CSV

      表  2  英云闪长岩围岩10 Ma后的不同熔融程度所对应的各项参数

      Table  2.   Parameters of different melting levels for tonalite after 10 Ma

      熔融程度(%) 温度(℃) 时间(Ma) 距离(km)
      0 850 10 3.108
      10 875 10 2.474
      20 900 10 1.850
      30 950 10 0.800
      38 1 000 10 0.120
      下载: 导出CSV

      表  3  玄武岩岩浆10 Ma后的不同结晶程度所对应的各项参数

      Table  3.   Parameters of different crystallization levels for basalt magma after 10 Ma

      熔融程度(%) 温度(℃) 时间(Ma) 距离(km)
      0 1 250 10 10.285
      10 1 225 10 8.739
      20 1 200 10 7.410
      30 1 150 10 6.950
      40 1 160 10 6.724
      50 1 175 10 6.296
      60 1 185 10 5.690
      70 1 190 10 5.306
      80 1 125 10 4.216
      90 1 100 10 3.448
      100 1 075 10 2.724
      下载: 导出CSV
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    出版历程
    • 收稿日期:  2011-10-19
    • 网络出版日期:  2021-11-15
    • 刊出日期:  2012-05-01

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