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A Kirchhoff migration imaging method based on grounded-source TEM virtual wave-fields and its applications

机译:基于接地源TEM虚拟波字段及其应用的基于基于接地源极的迁移成像方法

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This research study was based on a Kirchhoff migration imaging method, and the aim of the study was to realize grounded-source transient electromagnetic virtual wave-field migration. Diffusion equations mainly characterize the induction characteristics of low-frequency electromagnetic waves which are not suitable for wavefields. Wave equations mainly characterize wave reflections, refractions, and other propagation features, which are suitable for wave-field imaging processes. A unique mathematical transformation relationship exists between the diffusion fields of transient electromagnetic fields and seismic wave-fields. After the transformations from diffusion fields to virtual wave-fields are achieved, seismic interpretation methods can be used for the transient electromagnetic data interpretations. First, in order to realize Kirchhoff migration imaging based on transient electromagnetic wave-fields, precondition regularization methods are used for the wave-field inverse transformations. Then, after obtaining the wave-field data, dynamic correction methods are adopted to convert the grounded-source transient electromagnetic virtual wave-fields to quasi-seismic zero offset data. At that point, a Kirchhoff integral can be applied to realize the grounded-source transient electromagnetic quasi-seismic migration imaging. A theoretical model was used to test the method which was proposed in this study. The results showed that the Kirchhoff migration imaging was able to determine the geometric formations of underground dielectric interfaces, which fully demonstrated the applicability of the proposed method. Finally, migration imaging processing was performed on the data obtained from a mining area, and the imaging results were found to be consistent with the known geological data. Therefore, the feasibility of using a wave-field transform method and Kirchhoff migration imaging technology for grounded-source transient electromagnetic data interpretations was successfully
机译:该研究研究基于Kirchhoff迁移成像方法,研究的目的是实现接地源瞬态电磁虚拟波场迁移。扩散方程主要表征低频电磁波的诱导特性,这不适用于波场。波浪方程主要表征波反射,折射和其他传播特征,其适用于波场成像过程。瞬态电磁场和地震波场的扩散场之间存在唯一的数学变换关系。在实现从扩散场到虚拟波场的转换之后,可以使用地震解释方法用于瞬态电磁数据解释。首先,为了实现基于瞬态电磁波场的Kirchhoff迁移成像,前提是正则化方法用于波场逆变换。然后,在获得波场数据之后,采用动态校正方法将接地源瞬态电磁虚拟波场转换为准震源零偏移数据。此时,可以应用Kirchhoff积分来实现接地源瞬态电磁准偏置成像。理论模型用于测试本研究中提出的方法。结果表明,柯克霍夫迁移成像能够确定地下介电界面的几何形成,这完全证明了该方法的适用性。最后,对从挖掘区域获得的数据进行迁移成像处理,发现成像结果与已知的地质数据一致。因此,成功使用了用于接地源瞬态电磁数据解释的波场变换方法和Kirchhoff迁移成像技术的可行性

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