地震地质

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多元约束方法对2020年四川青白江Ms 5.1级地震构造研究

徐芳1,鲁人齐1,王帅2,江国焰1,龙锋3,王晓山4,苏鹏1,刘冠伸1   

  1. 1. 中国地震局地质研究所
    2.
    3. 四川省地震局
    4. 河北省地震局
  • 收稿日期:2021-01-15 修回日期:2021-04-27 发布日期:2021-09-26
  • 通讯作者: 鲁人齐
  • 基金资助:
    隐伏活动断层的定量研究与三维建模:以龙门山山前带为例;不同构造类型活动断裂三维建模关键技术及应用:多元约束条件下活动断裂几何形态与物性结构匹配技术—物性结构和断裂几何形态匹配

STUDY ON THE STRUCTURE OF THE QINGBAIJIANG Ms 5.1 EARTHQUAKE IN SICHUAN PROVINCE IN 2020 BY MULTIPLE CONSTRAINT METHOD

  • Received:2021-01-15 Revised:2021-04-27 Published:2021-09-26

摘要: 2020年2月3日,在四川省成都市青白江区发生Ms 5.1级地震,震中位于川西盆地的龙泉山断裂带北段。龙泉山断裂带北段有东、西两支断层,目前对本次地震的发震断层、地震成因与动力来源尚不清楚,导致难以深入分析和评估龙泉山地区潜在的地震风险。本次研究采用了多元约束方法,通过地球物理、地震学、大地测量学,结合构造地质学与断层相关褶皱理论,对青白江Ms 5.1级地震进行综合研究。人工地震反射剖面揭示了本次震中位置的基本构造特征,为发育在中下三叠统区域性滑脱层之上的逆冲断层和反冲断层组合;地震重定位结果显示震源矩心深度5km,表明本次地震与浅层断层活动有关;余震重定位主要集中分布于龙泉山断裂北段东支附近,东支断层产状与震源机制解一致。研究提取了震中附近的InSAR同震形变场,同震形变量最大可达4cm;地震造成的形变在震中西北部为隆起,东南部为凹陷,符合龙泉山断裂带北段东支断裂逆冲活动特征。本次研究通过多学科交叉的多元约束,对2020年青白江Ms 5.1级地震构造进行了详细分析,厘定了发震断层并探讨了可能的地震动力学背景,为龙泉山地区的断层活动性分析和地震风险评估提供一定依据。

关键词: 青白江Ms 5.1级地震, 地震反射剖面, 地震重定位, InSAR同震形变, 龙泉山断裂带

Abstract: On February 3, 2020, an Ms 5.1 earthquake occurred in Qingbaijiang District, Chengdu City, Sichuan Province, with the epicenter located in the northern part of Longquanshan fault zone of the Western Sichuan Basin. There are east and west branch faults in the north part of Longquanshan fault zone, the seismogenic fault, earthquake genesis and power source of this earthquake are not clear at present, which makes it difficult to deeply analyze and evaluate the potential earthquake risk in Longquanshan area. In this study, the multiple constraint method was used to comprehensively study the Qingbaijiang Ms5.1 earthquake through geophysics, seismology, geodesy, combined with structural geology and fault-related fold theory. In this paper, the basic structural features of the epicenter are revealed by using the artificial seismic reflection profile, there is a combination of a back-thrust fault and a thrust fault developed on the regional detachment layer of middle -lower Triassic. The result of seismic relocation shows that the focal depth is 5 km, which indicates that the earthquake is related to the activity of shallow faults. The aftershock relocation is mainly distributed near the east branch of the north Longquanshan fault zone, and the occurrence of the east branch is consistent with the focal mechanism solution. The coseismic deformation field of InSAR near the epicenter is extracted, and the maximum coseismic deformation is 4cm; the deformation caused by the earthquake is uplift in the northwest of the epicenter and depression in the southeast, which is in line with the characteristics of thrust activity of the east branch of the north Longquanshan fault zone. In this study, through multidisciplinary and multiple constraints, the Qingbaijiang Ms 5.1 earthquake structure in 2020 is analyzed in detail, the seismogenic fault is determined, and the possible seismic dynamic background is discussed, which provides a certain basis for fault activity analysis and seismic risk assessment in Longquanshan area.

Key words: Qingbaijiang Ms 5.1 earthquake, seismic reflection profile, seismic relocation, InSAR coseismic deformation field, Longquanshan fault zone