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地震 ›› 2022, Vol. 42 ›› Issue (2): 111-122.doi: 10.12196/j.issn.1000-3274.2022.02.009

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2020年阿拉斯加MW7.8地震断层滑动反演及其触发影响研究

王玉婷1, 王武星1, 周新2, 刘琦1, 朱雨菲1   

  1. 1.中国地震局地震预测研究所, 地震预测重点实验室, 北京 100036;
    2.应急管理部国家自然灾害防治研究院, 北京 100085
  • 收稿日期:2021-10-22 修回日期:2021-11-09 出版日期:2022-04-30 发布日期:2023-02-17
  • 通讯作者: 王武星, 研究员。 E-mail: bkwwx@ief.ac.cn
  • 作者简介:王玉婷(1998-), 女, 四川内江人, 硕士研究生, 主要从事地壳形变观测与动力学研究。
  • 基金资助:
    国家自然科学基金面上项目(42074091); 国家重点研发计划项目(2017YFC1500501)

Inversion of Fault Slip from the 2020 Alaska MW7.8 Earthquake and its Triggering Effects

WANG Yu-ting1, WANG Wu-xing1, ZHOU Xin2, LIU Qi1, ZHU Yu-Fei1   

  1. 1. Institute of Earthquake Forecasting, China Earthquake Administration, Beijing 100036, China;
    2. National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, China
  • Received:2021-10-22 Revised:2021-11-09 Online:2022-04-30 Published:2023-02-17

摘要: 2020年7月22日, 在北美板块和太平洋板块交界区的阿拉斯加半岛阿留申俯冲带上发生了MW7.8逆冲地震, 三个月后距震中西南80 km处发生了MW7.6走滑地震, 一年后距震中东南50 km处发生了MW8.2逆冲地震。 本文基于GPS同震形变, 利用非负最小二乘方法反演了MW7.8地震的断层同震破裂滑动分布, 研究其变形特征, 并基于地震位错理论计算了该地震对后续两个地震的库仑应力影响。 地震断层滑动反演结果显示地震矩为9.28×1020 N·m, 矩震级为MW7.8; 断层破裂滑移自震中沿断层向SWW向延伸, 在震中西南侧断层滑动量较大, 深度范围集中在25~45 km, 最大滑动量为2.26 m。 同震形变符合海沟特大地震的逆冲断层弹性回跳理论模式。 库仑应力变化计算结果显示2020年阿拉斯加MW7.8地震的库仑应力加载触发了MW7.6走滑地震, 并加速了2021年MW8.2逆冲地震的发生。

关键词: 2020年阿拉斯加MW7.8地震, 同震位移, 断层滑动分布, 库仑应力, 地震触发

Abstract: On July 22, 2020, an MW7.8 earthquake occurred in the Aleutian subduction zone of Alaska Peninsula at the junction of the North American plate and the Pacific plate. Three months later, the MW7.6 intraplate strike-slip aftershock occurred 80 km away from the epicenter in the Shumajin Gap. One year later, the MW8.2 earthquake occurred 50 km southeast of the epicenter. Based on GPS coseismic deformation, the approach of non-negative least squares was applied to inverse the fault rupture slip distribution of the earthquake. The result shows that the seismic moment is at about 9.28×1020 N·m, and the moment magnitude is MW7.8. The fault rupture slip extends from the epicenter along the fault to the SWW direction, and the magnitude of fault slip is larger in the southwest side of the epicenter. The depth range of the area with a large amount of slip is concentrated in the range of 25~45 km, and the maximum amount of slip is 2.26 m. This co-seismic deformation is consistent with the elastic rebound model of the subduction zone thrust fault. Coulomb stress results show that the 2020 MW7.8 earthquake in Alaska can trigger the thrust aftershocks, the MW7.6 strike-slip earthquake, and the 2021 MW8.2 thrust earthquake.

Key words: the 2020 Alaska MW7.8 earthquake, Coseismic displacement, Fault slip distribution, Coulomb stress, Earthquake triggering

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