2023年甘肃积石山MS6.2地震序列及发震构造分析

Analysis of earthquake sequence and seismogenic structure of the 2023 MS6.2 Jishishan earthquake,Gansu Province,China

  • 摘要: 2023年12月18日23时59分,甘肃省临夏州积石山县发生了MS6.2强震,震中位于柴达木—祁连地块东北缘拉脊山断裂系南段。本文基于地震重新定位与震源机制和应力反演结果对此次地震的发震构造进行了分析,并对区域危险性进行了初步探讨。采用甘肃和青海地震台网的观测数据,利用双差定位方法对震后10天的地震序列进行重定位,共获得605个高精度定位结果,结果显示主震震中位置为(35.748°N,102.812°E),震源深度为16.4 km。余震序列主要分布在6—15 km深度处,水平分布上,在震源区域内呈长轴沿NW−SE向展布,逐渐向北转变为近NS向展布,深度剖面显示出断层倾向为NE向。应用FocMech-Flow自动化流程反演震源机制解,获得MS6.2主震的最佳双力偶解,节面Ⅰ走向302°、倾角58°、滑动角45°;节面Ⅱ走向 184°、倾角53°、滑动角138°。其中,节面Ⅰ走向与震源区附近余震展布方向一致,可判定其为发震断层面。应力场反演结果表明震源区应力性质主要为逆冲型,最大主应力轴为WSW−ENE向。结合区域重力异常和已有地质资料,判断此次地震的发震断层为积石山东缘断裂系中的一条较深的反冲断层,并将其命名为“大河家断裂”。现有历史地震资料表明,近二十年来柴达木—祁连地块发生的强震具有向东迁移的趋势,此次地震的发生,暗示出位于积石山东部的西秦岭北缘断裂带未来的强震危险性有所增加。

     

    Abstract:
    On December 18th, 2023 at 23:59, an earthquake of MS6.2 occurred in Jishishan County, Linxia Prefecture, Gansu Province, with the epicenter located near the southern segment of the Lajishan fault system in the northeastern Qaidam-Qilian block. In this paper, we conducted the relocation, focal mechanism and stress inversion results to analyze the seismic structure and regional seismic risk. Using digital waveform data from the seismic networks of Gansu and Qinghai Provinces, the double-difference location algorithm was conducted on the earthquake sequence within 10 days after the earthquake.
    A total of 605 high-precision relocated earthquakes were revealed and the epicenter of the mainshock was determined to be at (35.748°E, 102.812°N), with a depth of 16.4 km. Most aftershocks located at depths of 6−15 km spreading along NW-SE direction near the mainshock epicenter, while some aftershocks gradually shift to a near NS direction to the north. Depth profile of aftershocks further suggests that the seismogenic fault plane dips to NE. By applying the FocMech-Flow automatic inversion of focal mechanism, the best double-couple solution for the MS6.2 mainshock was obtained. The parameters of two nodal planes are as follows: strike 302°, dip 58°, rake 45° for nodal plane I and strike 184°, dip 53°, rake 138° for nodal plane Ⅱ. Consistent with the direction of aftershock distribution near the mainshock, the plane Ⅰ is considered as the fault plane responsible for this earthquake. Stress field inversion results indicated that the stress in the epicenter belongs to thrust-type and the azimuth of σ1 axis orients WSW-ENE. Combining regional gravity anomaly and previous geological data, we suggest that the seismogenic fault is a deeply buried back thrust fault in the east Jishishan fault system and named it as “Dahejia fault”. Historical earthquake records in the Qaidam-Qilian block show that the strong earthquakes gradually migrate eastward in recent two decades. This earthquake further enhances the seismic hazards of the western Qinling fault to the east of Jishishan.

     

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