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Three-dimensional tensor controlled-source electromagnetic modeling based on the vectorfi nite-element method

机译:基于矢量有限元法的三维张量控制源电磁建模

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摘要

Scalar CSAMT is only suitable for measurements in one and two dimensions perpendicular to geological structures. For complex 3D geoelectric structure, tensor CSAMT is more suitable. In this paper, we discuss 3D tensor CSAMT forward modeling using the vector finite-element method. To verify the feasibility of the algorithm, we calculate the electric field, magnetic field, and tensor impedance of the 3D CSAMT far-zone field in layered media and compare them with theoretical solutions. In addition, a three-dimensional anomaly in half-space is also simulated, and the response characteristics of the impedance tensor and the apparent resistivity and impedance phase are analyzed. The results suggest that the vector finite-element method produces high-precision electromagnetic field and impedance tensor data, satisfies the electric field discontinuity, and does not require divergence correction using the vectorfi nite-element method.
机译:标量CSAMT仅适用于垂直于地质结构的一维和二维测量。对于复杂的3D地电结构,张量CSAMT更合适。在本文中,我们将讨论使用向量有限元方法的3D张量CSAMT正向建模。为了验证该算法的可行性,我们计算了分层介质中3D CSAMT远区场的电场,磁场和张量阻抗,并将其与理论解进行了比较。此外,还模拟了半空间中的三维异常,并分析了阻抗张量的响应特性以及视电阻率和阻抗相位。结果表明,矢量有限元法产生高精度的电磁场和阻抗张量数据,满足电场不连续性,并且不需要使用矢量有限元法进行发散校正。

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  • 来源
    《应用地球物理(英文版)》 |2015年第1期|35-46|共12页
  • 作者单位

    College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China;

    College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China;

    Tianjing Center, China Geological Survey, Tianjing 300170, China;

    Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, China;

    College of Geosciences and Technology, ShanDong University of Science and Technology, Qingdao 266590, China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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