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2008年汶川大地震孕震、同震及震后变形和应力演化全过程的数值模拟

孟秋, 高宽, 陈启志, 胡才博. 2021. 2008年汶川大地震孕震、同震及震后变形和应力演化全过程的数值模拟. 地质力学学报, 27(4): 614-627. doi: 10.12090/j.issn.1006-6616.2021.27.04.051
引用本文: 孟秋, 高宽, 陈启志, 胡才博. 2021. 2008年汶川大地震孕震、同震及震后变形和应力演化全过程的数值模拟. 地质力学学报, 27(4): 614-627. doi: 10.12090/j.issn.1006-6616.2021.27.04.051
MENG Qiu, GAO Kuan, CHEN Qizhi, HU Caibo. 2021. Seismogenic, coseismic and postseismic deformation and stress evolution of the 2008 Wenchuan earthquake: Numerical simulation analysis. Journal of Geomechanics, 27(4): 614-627. doi: 10.12090/j.issn.1006-6616.2021.27.04.051
Citation: MENG Qiu, GAO Kuan, CHEN Qizhi, HU Caibo. 2021. Seismogenic, coseismic and postseismic deformation and stress evolution of the 2008 Wenchuan earthquake: Numerical simulation analysis. Journal of Geomechanics, 27(4): 614-627. doi: 10.12090/j.issn.1006-6616.2021.27.04.051

2008年汶川大地震孕震、同震及震后变形和应力演化全过程的数值模拟

  • 基金项目:
    国家自然基金面上项目(42074117,41474085)
详细信息
    作者简介: 孟秋(1994-), 在读博士, 主要从事地球动力学数值模拟。E-mail: qmeng@whu.edu.cn
    通讯作者: 胡才博(1980-), 博士, 副教授, 主要从事地球动力学数值模拟。E-mail: hucb@ucas.ac.cn
  • 中图分类号: P313.2;P313.4;P313.5

Seismogenic, coseismic and postseismic deformation and stress evolution of the 2008 Wenchuan earthquake: Numerical simulation analysis

  • Fund Project: This research is financially supported by the National Natural Science Foundation of China (Grant No.42074117, 41474085)
More Information
  • 2008年MS 8.0级汶川大地震发生在具有复杂的地质构造背景、强烈的地表起伏、不均匀的弹性和黏性结构的龙门山断裂带上。由于震前地震活动性不够强烈且地表构造变形较小,龙门山断裂带的地震危险性在汶川地震之前被低估。从数值模拟的角度,建立黏弹性有限元模型,考虑了初始地形、重力、构造加载、黏弹性松弛等因素对2008年汶川大地震的孕震、同震及震后150年变形全过程的影响,定量研究了映秀-北川断裂带的同震及震后变形,分析了弹性层、黏弹性层的应力积累、释放、调整的特点,模拟得到地表同震和震后位移与大地测量资料较为吻合,对汶川大地震的余震分布进行了力学上的解释,模拟得到震前、同震及震后的应力变化有助于深入分析大地震的动力学成因及其对周围区域的地震危险性影响。

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  • 图 1  2008年汶川地震的地质构造背景和龙门山断裂带地表起伏图

    Figure 1. 

    图 2  有限元模型示意图

    Figure 2. 

    图 3  模型设定的初始位移和演化40万年之后的汶川地震初始位移

    Figure 3. 

    图 4  2008年汶川大地震的同震位移等值线图

    Figure 4. 

    图 5  2008年汶川大地震的地表同震位移分布

    Figure 5. 

    图 6  2008年汶川大地震引起的同震应力变化

    Figure 6. 

    图 7  2008年汶川大地震之后7年的震后位移(去掉同震位移后)

    Figure 7. 

    图 8  汶川大地震50年后的位移变化

    Figure 8. 

    图 9  汶川大地震100年后的位移变化

    Figure 9. 

    图 10  映秀-北川断裂带西侧出露点的震后位移随时间的变化曲线

    Figure 10. 

    图 11  映秀-北川断裂带东侧出露点的震后位移随时间的变化曲线

    Figure 11. 

    图 12  2008年汶川大地震平行于主震震源机制解主平面的同震结果

    Figure 12. 

    图 13  2008年汶川大地震平行于主震震源机制解主平面的震后50年结果

    Figure 13. 

    图 14  2008年汶川大地震的余震在剖面上的投影分布

    Figure 14. 

    表 1  龙门山断裂带两侧P波速度随深度的分布表(黄晓萍,2012)

    Table 1.  Distribution of P-wave velocity with depth on both sides of the Longmenshan fault zone (Huang, 2012)

    龙门山断裂带西侧(松潘甘孜地块) 龙门山断裂带东侧(四川盆地)
    界面深度/km P波速度/(km/s) 界面深度/km P波速度/(km/s)
    0 5.0 0 4.5
    4 5.4 3 5.0
    7 5.8 7 5.4
    10 6.0 10 6.0
    15 6.2 15 6.4
    30 6.4 25 6.8
    40 6.7 40 7.5
    50 6.9 50 8.0
    60 7.8 60 8.3
    70~100 8.3 70~100 8.3
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出版历程
收稿日期:  2020-11-30
修回日期:  2021-01-15
刊出日期:  2021-08-28

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