采用相关对比与人机交互对比相结合的方法确定地层微电阻率曲线之间的高程差；由高程差、井径和角度曲线求取层面在大地坐标系中的视倾斜矢量，通过视倾斜矢量在水平投影网中的投影确定地层的真倾角与方位。根据上述处理方法，编制了相应的处理软件，运用该软件处理的结果与实际地层情况完全一致。 The correlation between the contrast and human-computer interaction is used to determine the elevation difference between the micro-resistivity curves of the strata. The elevation gradient, the caliper and the angle curve are used to determine the apparent tilt vectors in the geodetic coordinate system. The projection in the horizontal projection network determines the true dip and azimuth of the formation. According to the above processing method, the corresponding processing software is compiled, and the result processed by the software is exactly the same with the actual formation.