Then inversion of the advanced detection is caried out by least square method. 然后采用最小二乘法對超前探測視電阻率曲線(xiàn)進(jìn)行快速反演。
The model parameters are estimated using a recursive extended least square method. 用遞歸擴展最小二乘法估算了模型參數。
Moreover, The authors inverted three dimensional global mantle density anomaly combining geoid data and seismic tomography data by means of damping least square method. 另外，采用阻尼最小二乘方法，利用全球地震層析成像資料和大地水準面異常資料聯(lián)合反演了三維全球地幔密度異常。
