利用徐州地震台四分量钻孔应变仪2009—2022年观测资料,基于力学转换和多尺度变化数据拟合,分析观测区域应力应变状态。结果表明,观测期间,该台测点附近区域呈稳定的受压状态,主应变变化速率稳定,最大和最小主应变年变化分别约为-4 132×10-10和-6 788×10-10,面应变和剪应变年变化分别约为10 919×10-10和1 328×10-10,应变变化主方向指向NE136°。结合潮汐调和分析法绘制潮汐因子响应图,发现四分量钻孔应变仪潮汐因子增大的长轴方向与最大主压应变方向基本一致,为准确判断区域应力状态提供了重要依据。选取GNSS数据分析江苏及邻区水平运动速度场,结果显示,江苏地区整体运动趋向SE,与四分量钻孔应变仪观测的应变变化主方向一致,进一步验证了徐州地震台钻孔应变观测数据的可靠性。
Using the four-component borehole strainmeter data collected by the Xuzhou Seismic Station from 2009 to 2022, this study analyzed the stress-strain state of the observation area through mechanical conversion and multiscale data fitting. The research results show that the observation area near the Xuzhou Station exhibited a stable over-pressured state during the observation period, with stable rates of change in principal strain. The annual change rates of maximum and minimum principal strain were approximately -4 132×10-10 and -6 788×10-10, respectively, while the annual change rates of plane strain and shear strain were approximately 10 919×10-10 and 1 328×10-10. The principal strain change direction was 136°. By combining the tide harmonic analysis diagram drawn using the Venetikov tidal harmonic analysis method, it was found that the direction of the tidal factor increase in the four-component borehole strainmeter was consistent with the direction of the maximum principal compressive strain calculated through fitting, providing important evidence for accurately judging the regional stress state. To analyze the stress field characteristics from a broader perspective, this study also used GNSS data to analyze the horizontal velocity field in Jiangsu and its neighboring regions. The GNSS analysis results show that Jiangsu as a whole exhibits a southeastward movement trend, which is consistent with the principal strain change direction observed by the four-component borehole strainmeter, further verifying the reliability of the observation data collected by the Xuzhou Station.
2024,45(5): 122-130 收稿日期:2024-5-17
DOI:10.3969/j.issn.1003-3246.2024.05.017
基金项目:连云港市科技局重点研发计划(社会发展)(项目编号:SF2326);江苏省地震局青年科研基金(项目编号:202412);江苏省地震局青年科研基金(项目编号:202413);中国地震局监测、预报、科研三结合项目(项目编号:3JH-202401039)
作者简介:郝冉(1991-),男,工程师,主要从事定点形变观测与研究工作。E-mail:haoran910106@163.com
参考文献:
陈永前,张淑亮,李宏伟. 基于四分量钻孔应变资料的区域应变场特征分析[J]. 大地测量与地球动力学,2021,41(10):1 095-1 100.
池顺良,武红岭,骆鸣津.钻孔应变观测中潮汐因子离散性与各向异性原因探讨——“十五”数字地震观测网络分量钻孔应变仪首批观测资料分析解释[J].地球物理学进展,2007,22(6):1 746-1 753.
顾勤平,康清清,许汉刚,等. 薄覆盖层地区隐伏断层及其上断点探测的地震方法技术——以废黄河断层为例[J].地球物理学报,2013,56(5):1 609-1 618.
江在森,马宗晋,张希,等. GPS初步结果揭示的中国大陆水平应变场与构造变形[J].地球物理学报,2003,46(3):352-358.
邱泽华,唐磊,郭燕平,等. 用四分量钻孔应变仪观测构造应变速率[J].地球物理学进展,2020,35(5):1 688-1 701.
邱泽华. 钻孔应变观测理论和应用[M]. 北京:地震出版社,2017.
唐磊,邱泽华,李玉江,等.四分量钻孔应变观测近地表应力应变状态的判定与分析[J/OL].武汉大学学报(信息科学版),2022.doi:10.13203/j.whugis20220397.
张凌空,牛安福. 分量式钻孔应变观测耦合系数的计算[J].地球物理学报,2013,56(9):3 029-3 037.