频率测深理论曲线现有计算公式都是把各层的磁导率看成等于真空磁导率μ_o的情况下推演出来的,这对沉积岩层通常是适宜的;但对磁导率较大的岩层(基性火成岩),将导致频率测深视电阻率值的增高。从这点出发,我们就磁导率对频率测深视电阻率曲 The existing calculation formulas of frequency sounding theoretical curves are derived from considering the permeability of each layer as equal to the vacuum permeability μ_o, which is usually suitable for sedimentary strata. However, for the large permeability Rock formations (basic igneous rocks) will result in an increase in apparent resistivity as a function of frequency. From this point of departure, we measured the permeability as a function of frequency as the resistivity