地震地质 ›› 2017, Vol. 39 ›› Issue (4): 837-852.DOI: 10.3969/j.issn.0253-4967.2017.04.016

• 问题讨论 • 上一篇    下一篇

三峡库区巴东地震前后视应力变化特征

戴苗1,2,3, 吴桂桔1, 刘坚1, 申重阳1, 孙少安1, 申学林1,2,3, 魏贵春1,2,3   

  1. 1 中国地震局地震研究所, 地震大地测量重点实验室, 武汉 430071;
    2 中国地震局地震研究所, 地震预警湖北省重点实验室, 武汉 430071;
    3 湖北省地震局, 武汉 430071
  • 收稿日期:2016-06-15 修回日期:2016-09-23 出版日期:2017-08-20 发布日期:2017-09-15
  • 通讯作者: 吴桂桔,副研究员,E-mail:wugjsky@126.com
  • 作者简介:戴苗,男,1982年生,2008年于中国地质大学获固体地球物理学硕士学位,工程师,主要从事测震学理论、方法和应用研究,E-mail:theocean123@163.com。
  • 基金资助:
    中国地震局地震研究所所长基金(201656264)与中国地震局测震台网青年骨干培养专项(20160516)共同资助

APPARENT STRESS VARIATION CHARACTERISTICS BEFORE AND AFTER BADONG EARTHQUAKE IN THE THREE GORGES RESERVOIR AREA

DAI Miao1,2,3, WU Gui-ju1, LIU Jian1, SHEN Chong-yang1, SHEN Xue-lin1, SHEN Xue-lin1,2,3, WEI Gui-chun1,2,3   

  1. 1 Key Laboratory of Earthquake Geodesy, Institute of Seismology, China Earthquake Administration, Wuhan 430071, China;
    2 Hubei Key Laboratory of Earthquake Early Warning, Institute of Seismology, China Earthquake Administration, Wuhan 430071, China;
    3 Earthquake Administration of Hubei Province, Wuhan 430071, China
  • Received:2016-06-15 Revised:2016-09-23 Online:2017-08-20 Published:2017-09-15

摘要: 三峡库区地震成因复杂,为了研究该区域地震的成因及发震规律,文中利用湖北省区域台网、三峡台网提供的数字波形资料,计算2010年1月1日至2015年12月31日三峡库区394个ML ≥ 2.0地震的震源参数,获得了三峡库区视应力的时空分布图像,分析了三峡库区研究时间段显著地震事件前后的视应力时空演化特征。研究表明:1)巴东ML5.5、秭归ML4.7以及ML5.1地震发生前后,不同震级分段计算结果显示,震前震中区附近新华-水田坝断裂和高桥断裂同时出现高值,高值区域分布呈现协同化程度高,而震后零散的现象,表明该区域在震前积累了较高的应力。2)研究区域视应力在地震前后经历了一个明显的"上升-下降"过程,在应力上升初期发生了巴东ML5.5、秭归ML4.7以及ML5.1三次显著地震。3)研究区域视应力深度剖面显示,不同深度视应力与震级大小呈现正相关性,震后研究区内小震属于低应变释放背景下的低应力释放,未新增明显视应力异常集中区域,震后巴东高桥断裂、周家山-牛口断裂以及秭归仙女山断裂短期内发生破坏性地震的可能性不大。

关键词: 视应力, 时空特征, 三峡库区, 巴东地震

Abstract: The causes of earthquakes in the Three Gorges reservoir area are complex. In order to study the cause of earthquakes happening in the region, we calculated the source parameters of 394 ML ≥ 2.0 earthquakes occurring in Three Gorges reservoir area based on waveform data observed by the regional seismic network of Hubei Province and Three Gorges, obtained the apparent stress spatial-temporal variation map of Three Gorges reservoir area, and analyzed apparent stress spatial-temporal variation characteristics before and after the main earthquakes in the Three Gorges reservoir area. The results show that:1)Before the Badong ML5.5, Zigui ML4.7 and Zigui ML5.1 earthquake, high apparent stress of earthquakes with different magnitudes is concentrated in Xinhua-Shuitianba Fault and Gaoqiao Fault. The distribution of high value area shows the high degree of synergism before the earthquake and the scattering after the earthquake, which indicates that the area accumulated a high stress before the earthquake, and the fault was in a locked state; 2)In the study area, the apparent stress before and after the earthquake showed significant rise in the first and then decline, the earthquake occurred in the process of rising; 3)Apparent stress depth profiles show that apparent stress at different depths has a positive correlation with the size of magnitude of earthquake, and the phenomenon of "small magnitude and strong apparent stress" did not appear. The small earthquakes occurring after the major earthquakes in the study area belong to low strain release under the background of low stress release, and there are no new apparent stress anomaly concentration areas appearing, this indicates that the Badong-Gaoqiao Fault, Zhoujiashan-Niukou Fault and Zigui Xiannushan Fault have been effective in releasing after the Badong earthquake and Zigui earthquakes and the probability of destructive earthquake is small on these faults.

Key words: apparent stress, spatial-temporal feature, Three Gorges, Badong earthquake

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