2022年1月2日云南宁蒗MS5.5地震矩张量及发震构造研究

刘俊清, 张宇, 蔡宏雷, 张雪冰, 王光明, 陈兆新. 2025. 2022年1月2日云南宁蒗MS5.5地震矩张量及发震构造研究. 地球物理学报, 68(9): 3433-3445, doi: 10.6038/cjg2024S0468
引用本文: 刘俊清, 张宇, 蔡宏雷, 张雪冰, 王光明, 陈兆新. 2025. 2022年1月2日云南宁蒗MS5.5地震矩张量及发震构造研究. 地球物理学报, 68(9): 3433-3445, doi: 10.6038/cjg2024S0468
LIU JunQing, ZHANG Yu, CAI HongLei, ZHANG XueBing, WANG GuangMing, CHEN ZhaoXin. 2025. Study on the moment tensor and seismogenic tectonic of the Ninglang MS5.5 Earthquake on January 2, 2022, Yunnan Province. Chinese Journal of Geophysics (in Chinese), 68(9): 3433-3445, doi: 10.6038/cjg2024S0468
Citation: LIU JunQing, ZHANG Yu, CAI HongLei, ZHANG XueBing, WANG GuangMing, CHEN ZhaoXin. 2025. Study on the moment tensor and seismogenic tectonic of the Ninglang MS5.5 Earthquake on January 2, 2022, Yunnan Province. Chinese Journal of Geophysics (in Chinese), 68(9): 3433-3445, doi: 10.6038/cjg2024S0468

2022年1月2日云南宁蒗MS5.5地震矩张量及发震构造研究

  • 基金项目:

    吉林省科技发展计划项目(YDZJ202501ZYTS476)资助.

详细信息
    作者简介:

    刘俊清,男,副教授,主要从事地震活动性研究. E-mian:liujq9@126.com

    通讯作者: 陈兆新,男,工程师,主要从事地震活动性研究. E-mail:czx19902024@163.com
  • 中图分类号: P315

Study on the moment tensor and seismogenic tectonic of the Ninglang MS5.5 Earthquake on January 2, 2022, Yunnan Province

More Information
  • 基于云南和四川区域地震台网的数字地震观测资料,采用矩心矩张量反演方法,结合断层失稳参数,对2022年1月2日发生在云南宁蒗的MS5.5地震的震源机制和发震构造进行研究. 结果显示,宁蒗MS5.5地震破裂过程由两个在时间和空间上独立的子地震组成:较大子地震Mmajor占总地震矩的74.7%,矩震级为MW5.2,较小子地震Mminor占总地震矩的25.3%,矩震级为MW4.9,二者均为典型的正断层地震. 断层失稳参数分析显示,Mmajor震源机制解中的节面I对应的断裂,即走向NW、倾向NE的永宁断裂推测其为主发震断裂. 较大余震的震源机制解表明,主震激发了震中区附近的次级断裂的活动. 研究认为,2022年宁蒗MS5.5地震是在区域构造应力场的作用下,永宁断裂继2012年6月24日宁蒗—盐源MS5.7地震后,沿NW方向进一步扩展的结果,反映出该断裂在过去十年中持续积累应力并发生破裂的构造演化特征.

  • 加载中
  • 图 1 

    地震构造与M-T

    Figure 1. 

    Seismotectonic setting and M-T plot

    图 2 

    地壳速度模型和CMT反演结果

    Figure 2. 

    Crustal velocity models and CMT inversion results

    图 3 

    偏矩张量反演波形拟合图

    Figure 3. 

    Waveform fitting from Deviatoric MT inversion

    图 4 

    矩张量分量不确定度评估

    Figure 4. 

    Uncertainty assessment of the components of the MT

    图 5 

    偏矩张量解分解(沙滩球直径与M0成正比)

    Figure 5. 

    Decomposition of the Deviatoric MT solution (The radius of the beach ball is proportional to M0.)

    图 6 

    多点源地震矩张量反演结果

    Figure 6. 

    Results of the multiple-point source MT inversion

    图 7 

    滇西北构造应力场应力莫尔圆与地震震源机制解节面投影

    Figure 7. 

    Mohr circle diagram of tectonic stress field in Northwestern Yunnan and projection of the nodal plane of the focal mechanism solution

    表 1 

    2022年宁蒗5.5级主震和余震定位

    Table 1. 

    Location of Ninglang MS5.5 mainshock and aftershocks on 2022

    MS Date Time Depth(km) Lontitude(°) Latitude(°)
    5.5 2022-01-02 15:02:07 10 100.65 27.79
    4.4 2022-01-05 17:52:49 6 100.64 27.84
    4.6 2022-04-16 08:32:14 9 100.62 27.77
    4.2 2022-04-17 00:18:37 8 100.61 27.75
    4.3 2022-04-30 01:23:49 8 100.61 27.77
    下载: 导出CSV

    表 2 

    地壳速度模型与VR值

    Table 2. 

    Crustal velocity models and VR values

    VR(DC)VR(Deviatoric MT)VR(Full MT)
    VM-172%82%82%
    VM-272%82%82%
    VM-368%76%76%
    下载: 导出CSV

    表 3 

    2022年宁蒗5.5级地震全矩张量反演结果

    Table 3. 

    Full MT inversion results for the 2022 Ninglang MS5.5 earthquake

    Item Value
    Centroid: Lat./Lon./Depth 27.79°/100.65°/3 km
    Centroid time (hh:mm:ss.s) 15:02:11.4
    M0/MW 9.577 × 1016 N·m / 5.29
    Nodal Plane-I: Strike/Dip/Rake 299°/71°/-158°
    Nodal Plane-II: Strike/Dip/Rake 201°/70°/-20°
    Uncertainty (2σ): Strike/Dip/Rake 1.0°/2.2°/2.0°
    DC/CLVD/ISO 56.5%/40.2%/3.3%
    Uncertainty (2σ): DC/CLVD/ISO 3.8%/6.0%/3.0%
    M [Mrr/Mtt/Mpp/Mrt/Mrp/Mtp] [-2.19/-3.32/10.55/2.40/0.54/-5.8]
    × 1016 N·m
    下载: 导出CSV

    表 4 

    偏矩张量解分解结果

    Table 4. 

    Results of deviatoric MT decomposition

    Sub-event Nodal Plane-I
    Strike/Dip/Rake (°)
    Nodal Plane-II
    Strike/Dip/Rake (°)
    M0(%) M0(N·m) MW
    Mmajor 306/59/-143 194/59/-37 74.7 7.154 × 1016 5.2
    Mminor 124/61/-147 16/61/-33 25.3 2.423 × 1016 4.9
    下载: 导出CSV

    表 5 

    余震矩张量反演结果

    Table 5. 

    Moment tensor inversion results of the aftershocks

    MS MW Centroid
    Depth(km)
    VR
    (%)
    DC
    (%)
    CLVD
    (%)
    Strike/Dip/Rake(°) P-axis
    Azimuth/Plunge(°)
    T-axis
    Azimuth/Plunge(°)
    4.4 4.3 4 62 97.6 -2.4 325/41/-103
    161/50/-79
    124/81 244/5
    4.6 4.6 4 77 92.2 -7.8 270/89/-175
    180/85/-1
    135/4 45/3
    4.2 4.4 4 65 85.8 -14.2 92/81/177
    183/87/9
    317/4 48/9
    4.3 4.4 5 73 85.9 -14.1 92/80/-179
    2/89/-10
    316/8 47/6
    下载: 导出CSV

    表 6 

    震源机制解节面的失稳参数

    Table 6. 

    Instability parameters of the nodal plane in the focal mechanism solution

    Date MS Nodal Plane-I
    Strike/Dip/Rake (°)
    I Nodal Plane-II
    Strike/Dip/Rake (°)
    I
    2022-01-02 MmajorMW 5.2 306/59/-143 0.9820 194/59/-37 0.3648
    MminorMW 4.9 124/61/-147 0.7475 16/61/-33 0.7521
    2022-01-05 4.4 325/41/-103 0.9691 161/50/-79 0.5567
    2022-04-16 4.6 180/85/-1 0.8332 270/89/-175 0.7001
    2022-04-17 4.2 183/87/9 0.8120 92/81/177 0.6505
    2022-04-30 4.3 2/89/-10 0.8518 92/80/-179 0.6441
    2012-06-24 5.7 302/55/-141 0.9896 189/59/-40 0.4355
    注:粗体数字表示区域应力场触发的发震断裂产状和对应的失稳参数值.
    下载: 导出CSV
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出版历程
收稿日期:  2024-08-06
修回日期:  2024-10-25
上线日期:  2025-09-01

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