根据捷克和斯洛伐克电磁台站的数据 ,得到波西米亚块体地壳和上地幔的电阻率分布模型。估计电阻率时特别使用了短周期和长周期的电磁数据以及用连续谱方法对固定台站数据的分析结果。根据欧洲地磁感应矢量分布绘出了显著的地电不均匀带的地图 ,将波西米亚块体的视电阻率与中欧有关台站的感应标量长度与W1响应做了比较 ,并根据电阻率 /深度图估计了电导率范围 ,该图与替代性理想导体反演相对应。 According to the data from Czech and Slovakia electromagnetic stations, the resistivity distribution model of the Bohemia crust and the upper mantle is obtained. In particular, short-period and long-period electromagnetic data are used in the estimation of the resistivity and the results of the analysis of the data of the fixed station by the continuous spectrum method are used. According to the geomagnetic induction vector distribution in Europe, a significant map of the geoelectric uneven band is drawn. The apparent resistivity of the Bohemia block is compared with that of the relevant stations in Central Europe and the W1 response. According to the resistivity The depth map estimates the conductivity range, which corresponds to the alternative ideal conductor inversion.