给出直流电阻率、激发极化测深法数据的二维有限元反演方法和原理。
The method and principle of 2-d structure finite element inversion for resistivity and IP data is presented.
水底极化体有限元正演模拟的结果表明，水底地形对激发极化测深结果没有影响。
The results of numerical modeling of subaqueous induced polarization show that the topographic don't have influence on the section of IP sounding.
激发极化法的探测深度可达数千米深。
The IP method can probe to subsurface depths of thousands of meters.
激发极化法的探测深度可达数千米深。
The IP method can probe to subsurface depths of thousands of meters.
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