The probability tomography of electromagnetic field-derivative method is an imaging inversion method that emphasizes particularly on singling out the anomaly.
电磁导数场概率成像方法是一种侧重于识别地质异常体的成像反演方法。
The results observed show that electromagnetic wave anomaly can be regarded as a shortterm and imminent predicting index of earthquake.
观测结果表明，电磁波异常可以作为一种地震的短临预报指标。
We present a mesh convergence test of the 3-d finite difference method for computing the electromagnetic response of a buried conductivity anomaly.
本文用三维有限差分法，在计算电导率异常的电磁响应时作了一次网格收敛试验。
We present a mesh convergence test of the 3-d finite difference method for computing the electromagnetic response of a buried conductivity anomaly.
本文用三维有限差分法，在计算电导率异常的电磁响应时作了一次网格收敛试验。
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