地震地质

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首都圈极低频电磁台网区地下电性结构探测

董泽义1,汤吉1,赵国泽1,陈小斌1,2,崔腾发1,韩冰1,姜峰3,王立凤1   

  1. 1. 中国地震局地质研究所
    2. 应急管理部国家自然灾害防治研究院
    3. 南方科技大学
  • 收稿日期:2021-05-06 修回日期:2021-09-28 发布日期:2021-12-09
  • 通讯作者: 汤吉
  • 基金资助:
    国家重大科学技术设施项目《极低频探地(WEM)工程》地震预测分系统;国家自然科学基金项目

PROBING THE SUBSURFACE ELECTRIC STRUCTURE FOR CSELF NETWORK IN CAPITAL CIRCLE REGION

  • Received:2021-05-06 Revised:2021-09-28 Published:2021-12-09
  • Contact: Ji 无Tang

摘要: 开展极低频电磁(CSELF)台网区/台站的地下背景电性结构探测对于发挥它在地震预测预报研究中的作用具有重要意义。本研究在首都圈CSELF电磁台网的每个台站附近布设了一条短的宽频带大地电磁剖面,共完成了60个测点的数据采集,对数据进行了处理与分析,首先采用大地电磁一维反演获得了每个台站和测点下方的电阻率结构,然后利用二维反演技术获得了每个台站沿剖面的地壳电性结构,最后对整个台网区的台站数据进行了三维反演,获得了台网区三维地壳电性结构。结果表明,华北北部阴山-燕山造山带、中部的太行山地区和东部的胶-辽地块地壳电性结构主要表现为高阻特征,华北平原和山西断陷区域表现为相对低阻;太行山重力梯度带与郯庐断裂带两侧的电性结构差异明显,表现为电性边界带;台网区的电性结构特征与区域地质构造、地震活动性特征具有明显的相关性。首都圈CSELF台网区地下电性结构探测为区域的孕震环境、地震电磁异常信号产生机理以及地震预测预报研究工作提供了重要的参考资料。

关键词: 首都圈, 极低频电磁台网, 大地电磁, 电性结构

Abstract: Carrying out the detection of the underground background electric structure in the CSELF network area/station is of great significance to play its role in the study of earthquake prediction and forecast. A short magnetotelluric (MT) profile was deployed at each station of the CSELF network in the Capital Circle region and a total of 60 broadband MT sites was collected using ADU-07e systems. All the time series data were processed to MT transfer functions and analyzed in detail with different impedance tensor decomposed methods. On the one hand, one-dimensional (1D) subsurface electrical resistivity structures at each station and MT site were derived from 1D MT inversion. On the other hand, we also imaged the electric structures along the short MT profile by 2D inversion at each station. In addition, the 3D inversion of 15 stations was performed to produce a 3-D crustal electrical resistivity model for the entire network. The combined results show: the crustal electrical structures are mainly characterized by high resistivity beneath the Yinshan-Yanshan orogenic belt in the north of North China, the Taihangshan area in the middle, the Jiao-Liao block in the east, while the North China Plain and Shanxi depression areas have relatively lower resistivity in the crust; There are obvious electrical resistivity difference on both sides of the gravity gradient of Taihang Mountain and the Tanlu fault zone, which indicates they could be manifested as an electric structure boundary zone, respectively. The electric structure characteristics of the entire network area are related to the regional geological structure and seismic activity to some extent. Implementing the detection of the underground electrical resistivity structure in the CSELF network of the Capital Circle region will provide important foundations for the researches on the regional seismogenic, the generation mechanism of seismic electromagnetic anomaly signals, and earthquake prediction and forecast.

Key words: Capital Circle Region, CSELF network, magnetotelluric, electric structure