2025年12月4日新疆阿合奇6.0级地震应急产品及震源参数初步分析
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P315

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Preliminary Analysis of Emergency Production and Source Parameters of the M6.0 Earthquake on December 04,2025 in Aheqi,Xinjiang
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    摘要:

    北京时间2025年12月4日15时44分,新疆克孜勒苏州阿合奇县(41.13°N,78.40°E)发生6.0级地震,中国地震预警网于震后7.9s产出首报预警结果; 中国地震台网中心于震后141s发布自动速报结果、震后15min发布正式速报结果,同时联合多家单位启动地震应急产品产出工作,共产出震源参数、地震构造、历史地震、震源机制、震源破裂过程和地震烈度等应急产品。结果显示,认为本次地震发生在迈丹—沙依拉姆断裂附近,该区域地质构造活跃; 根据震源机制解反演结果,本次地震是一次以逆冲为主的事件,这与该区域多数历史地震的类型特征保持一致; 破裂过程结果显示余震展布呈近NE向,与震中区域断裂走向基本一致; 烈度速报推测极震区烈度达Ⅷ度,区域面积约98km2

    Abstract:

    At 15:44 Beijing time on December 4,2025,a magnitude 6.0 earthquake struck Aheqi County,Kizilsu Kirghiz Autonomous Prefecture,Xinjiang(41.13°N,78.40°E). the China Earthquake Early Warning Network issued its first early warning results 7.9s after the earthquake and released the automatic rapid report 141s after the event. the China Earthquake Networks Center published the official rapid report 15min after the earthquake. Emergency response products were subsequently generated in collaboration with other institutes,including source parameters,seismotectonic background,historical seismicity,focal mechanism,rupture process,and estimated intensity. the results indicate that the earthquake occurred near the Maidan-Shayilamu Fault,where tectonic activity is strong. Focal mechanism inversion shows that the event was dominated by thrust faulting,consistent with the focal mechanism characteristics of most historical earthquakes in the region. Rupture process inversion reveals that the slip distribution was generally oriented in a near-NE direction,broadly consistent with the strike of faults in the epicentral area. the rapid intensity report indicates that the maximum intensity in the epicentral area reached VIII,with an affected area of approximately 98km2.

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冯凡,戴丹青,杨志高,徐泰然,席楠,孙丽.2025年12月4日新疆阿合奇6.0级地震应急产品及震源参数初步分析[J].中国地震,2026,42(1):217-226

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  • 收稿日期:2025-12-23
  • 最后修改日期:2026-02-02
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  • 在线发布日期: 2026-05-28
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